---
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '19672'
abstract:
- lang: eng
  text: 'Some of the classical models of tropical cyclone intensification predict
    tropical cyclones to intensify up to a steady intensity, which depends on surface
    fluxes only, without any relevant role played by convective motions in the troposphere,
    typically assumed to have a moist adiabatic lapse rate. Simulations performed
    using the non-hydrostatic, high-resolution model System for Atmosphere Modeling
    in idealized settings (rotating radiative-convective equilibrium on a doubly periodic
    domain) show early intensification consistent with these theoretical expectations,
    but different intensity evolution, with the cyclone undergoing an oscillation
    in wind speed. This oscillation can be linked to feedbacks between the cyclone
    intensity and air buoyancy: convective heating, radiative heating, and mixing
    with warm low stratospheric air warm the mid and upper troposphere of the cyclone
    stabilizing the air column and thus reducing its intensity. After the intensity
    decay phase, mid and upper tropospheric cooling, mostly through cold advection
    from the surroundings, cooled by radiation, rebuilds Convective Available Potential
    Energy, that peaks just before a new intensification phase. These idealized simulations
    thus highlight the potentially important interactions between a tropical cyclone,
    its environment and radiation.'
acknowledgement: The authors acknowledge two anonymous reviewers and the editor who
  provided insightful remarks and comments that helped to significantly improve the
  manuscript. AP and CJM gratefully acknowledges funding from the European Research
  Council (ERC) under the European Union's Horizon 2020 research and innovation program
  (Project CLUSTER, Grant Agreement No. 805041). Part of this work is an outcome of
  the project MIUR—Dipartimenti di Eccellenza 2023–2027. ANM is supported by HPC-TRES
  Grant 2023-04.
article_number: e2024MS004613
article_processing_charge: Yes
article_type: original
author:
- first_name: Andrea
  full_name: Polesello, Andrea
  id: 74c777f4-32da-11ee-b498-874db0835561
  last_name: Polesello
- first_name: Giousef Alexandros
  full_name: Charinti, Giousef Alexandros
  id: 7f7cc04c-074c-11ed-af92-eb16afd85c75
  last_name: Charinti
- first_name: Agostino Niyonkuru
  full_name: Meroni, Agostino Niyonkuru
  last_name: Meroni
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
- first_name: Claudia
  full_name: Pasquero, Claudia
  last_name: Pasquero
citation:
  ama: 'Polesello A, Charinti GA, Meroni AN, Muller CJ, Pasquero C. Intensity oscillations
    of tropical cyclones: Surface versus mid and upper tropospheric processes. <i>Journal
    of Advances in Modeling Earth Systems</i>. 2025;17(4). doi:<a href="https://doi.org/10.1029/2024MS004613">10.1029/2024MS004613</a>'
  apa: 'Polesello, A., Charinti, G. A., Meroni, A. N., Muller, C. J., &#38; Pasquero,
    C. (2025). Intensity oscillations of tropical cyclones: Surface versus mid and
    upper tropospheric processes. <i>Journal of Advances in Modeling Earth Systems</i>.
    Wiley. <a href="https://doi.org/10.1029/2024MS004613">https://doi.org/10.1029/2024MS004613</a>'
  chicago: 'Polesello, Andrea, Giousef Alexandros Charinti, Agostino Niyonkuru Meroni,
    Caroline J Muller, and Claudia Pasquero. “Intensity Oscillations of Tropical Cyclones:
    Surface versus Mid and Upper Tropospheric Processes.” <i>Journal of Advances in
    Modeling Earth Systems</i>. Wiley, 2025. <a href="https://doi.org/10.1029/2024MS004613">https://doi.org/10.1029/2024MS004613</a>.'
  ieee: 'A. Polesello, G. A. Charinti, A. N. Meroni, C. J. Muller, and C. Pasquero,
    “Intensity oscillations of tropical cyclones: Surface versus mid and upper tropospheric
    processes,” <i>Journal of Advances in Modeling Earth Systems</i>, vol. 17, no.
    4. Wiley, 2025.'
  ista: 'Polesello A, Charinti GA, Meroni AN, Muller CJ, Pasquero C. 2025. Intensity
    oscillations of tropical cyclones: Surface versus mid and upper tropospheric processes.
    Journal of Advances in Modeling Earth Systems. 17(4), e2024MS004613.'
  mla: 'Polesello, Andrea, et al. “Intensity Oscillations of Tropical Cyclones: Surface
    versus Mid and Upper Tropospheric Processes.” <i>Journal of Advances in Modeling
    Earth Systems</i>, vol. 17, no. 4, e2024MS004613, Wiley, 2025, doi:<a href="https://doi.org/10.1029/2024MS004613">10.1029/2024MS004613</a>.'
  short: A. Polesello, G.A. Charinti, A.N. Meroni, C.J. Muller, C. Pasquero, Journal
    of Advances in Modeling Earth Systems 17 (2025).
corr_author: '1'
date_created: 2025-05-11T22:02:41Z
date_published: 2025-04-01T00:00:00Z
date_updated: 2025-09-30T12:30:29Z
day: '01'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2024MS004613
ec_funded: 1
external_id:
  isi:
  - '001472439600001'
file:
- access_level: open_access
  checksum: 2f7c74aceaeea4be1fff4de300791319
  content_type: application/pdf
  creator: dernst
  date_created: 2025-05-12T12:17:08Z
  date_updated: 2025-05-12T12:17:08Z
  file_id: '19683'
  file_name: 2025_JAMES_Polesello.pdf
  file_size: 942325
  relation: main_file
  success: 1
file_date_updated: 2025-05-12T12:17:08Z
has_accepted_license: '1'
intvolume: '        17'
isi: 1
issue: '4'
language:
- iso: eng
license: https://creativecommons.org/licenses/by/4.0/
month: '04'
oa: 1
oa_version: Published Version
project:
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Journal of Advances in Modeling Earth Systems
publication_identifier:
  eissn:
  - 1942-2466
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: 'Intensity oscillations of tropical cyclones: Surface versus mid and upper
  tropospheric processes'
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 17
year: '2025'
...
---
OA_place: publisher
OA_type: hybrid
PlanS_conform: '1'
_id: '20705'
abstract:
- lang: eng
  text: Optical tweezers are widely used as a highly sensitive tool to measure forces
    on micron-scale particles. One such application is the measurement of the electric
    charge of a particle, which can be done with high precision in liquids, air, or
    vacuum. We experimentally investigate how the trapping laser itself can electrically
    charge such a particle, in our case a ∼1  μ⁢m SiO2 sphere in air. We model the
    charging mechanism as a two-photon process which reproduces the experimental data
    with high fidelity.
acknowledged_ssus:
- _id: M-Shop
- _id: ScienComp
acknowledgement: We thank Todor Asenov and Abdulhamid Baghdadi for their outstanding
  technical support and Dr. Michael Gleichweit and Mercede Azizbaig Mohajer for the
  helpful discussions. This project has received funding from the European Research
  Council (ERC) under the European Union’s Horizon 2020 research and innovation programme
  (Grant Agreements No. 949120 and No. 805041) and the Swiss National Science Foundation
  (SNSF, Project No. 200021-236446). This research was supported by the Scientific
  Service Units of the Institute of Science and Technology Austria (ISTA) through
  resources provided by the Miba Machine Shop and the Scientific Computing service
  unit.
article_number: '218202'
article_processing_charge: Yes (via OA deal)
article_type: original
arxiv: 1
author:
- first_name: Andrea
  full_name: Stöllner, Andrea
  id: 4bdcf7f6-eb97-11eb-a6c2-9981bbdc3bed
  last_name: Stöllner
  orcid: 0000-0002-0464-8440
- first_name: Isaac C
  full_name: Lenton, Isaac C
  id: a550210f-223c-11ec-8182-e2d45e817efb
  last_name: Lenton
  orcid: 0000-0002-5010-6984
- first_name: Artem
  full_name: Volosniev, Artem
  id: 37D278BC-F248-11E8-B48F-1D18A9856A87
  last_name: Volosniev
  orcid: 0000-0003-0393-5525
- first_name: James
  full_name: Millen, James
  last_name: Millen
- first_name: Renjiro
  full_name: Shibuya, Renjiro
  last_name: Shibuya
- first_name: Hisao
  full_name: Ishii, Hisao
  last_name: Ishii
- first_name: Dmytro
  full_name: Rak, Dmytro
  id: 70313b46-47c2-11ec-9e88-cd79101918fe
  last_name: Rak
- first_name: Zhanybek
  full_name: Alpichshev, Zhanybek
  id: 45E67A2A-F248-11E8-B48F-1D18A9856A87
  last_name: Alpichshev
  orcid: 0000-0002-7183-5203
- first_name: Grégory
  full_name: David, Grégory
  last_name: David
- first_name: Ruth
  full_name: Signorell, Ruth
  last_name: Signorell
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
- first_name: Scott R
  full_name: Waitukaitis, Scott R
  id: 3A1FFC16-F248-11E8-B48F-1D18A9856A87
  last_name: Waitukaitis
  orcid: 0000-0002-2299-3176
citation:
  ama: Stöllner A, Lenton IC, Volosniev A, et al. Using optical tweezers to simultaneously
    trap, charge, and measure the charge of a microparticle in air. <i>Physical Review
    Letters</i>. 2025;135(21). doi:<a href="https://doi.org/10.1103/5xd9-4tjj">10.1103/5xd9-4tjj</a>
  apa: Stöllner, A., Lenton, I. C., Volosniev, A., Millen, J., Shibuya, R., Ishii,
    H., … Waitukaitis, S. R. (2025). Using optical tweezers to simultaneously trap,
    charge, and measure the charge of a microparticle in air. <i>Physical Review Letters</i>.
    American Physical Society. <a href="https://doi.org/10.1103/5xd9-4tjj">https://doi.org/10.1103/5xd9-4tjj</a>
  chicago: Stöllner, Andrea, Isaac C Lenton, Artem Volosniev, James Millen, Renjiro
    Shibuya, Hisao Ishii, Dmytro Rak, et al. “Using Optical Tweezers to Simultaneously
    Trap, Charge, and Measure the Charge of a Microparticle in Air.” <i>Physical Review
    Letters</i>. American Physical Society, 2025. <a href="https://doi.org/10.1103/5xd9-4tjj">https://doi.org/10.1103/5xd9-4tjj</a>.
  ieee: A. Stöllner <i>et al.</i>, “Using optical tweezers to simultaneously trap,
    charge, and measure the charge of a microparticle in air,” <i>Physical Review
    Letters</i>, vol. 135, no. 21. American Physical Society, 2025.
  ista: Stöllner A, Lenton IC, Volosniev A, Millen J, Shibuya R, Ishii H, Rak D, Alpichshev
    Z, David G, Signorell R, Muller CJ, Waitukaitis SR. 2025. Using optical tweezers
    to simultaneously trap, charge, and measure the charge of a microparticle in air.
    Physical Review Letters. 135(21), 218202.
  mla: Stöllner, Andrea, et al. “Using Optical Tweezers to Simultaneously Trap, Charge,
    and Measure the Charge of a Microparticle in Air.” <i>Physical Review Letters</i>,
    vol. 135, no. 21, 218202, American Physical Society, 2025, doi:<a href="https://doi.org/10.1103/5xd9-4tjj">10.1103/5xd9-4tjj</a>.
  short: A. Stöllner, I.C. Lenton, A. Volosniev, J. Millen, R. Shibuya, H. Ishii,
    D. Rak, Z. Alpichshev, G. David, R. Signorell, C.J. Muller, S.R. Waitukaitis,
    Physical Review Letters 135 (2025).
corr_author: '1'
date_created: 2025-11-30T23:02:07Z
date_published: 2025-11-21T00:00:00Z
date_updated: 2026-04-28T13:09:27Z
day: '21'
ddc:
- '530'
- '550'
department:
- _id: ZhAl
- _id: CaMu
- _id: ScWa
doi: 10.1103/5xd9-4tjj
ec_funded: 1
external_id:
  arxiv:
  - '2507.17591'
file:
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  date_created: 2025-12-01T08:19:46Z
  date_updated: 2025-12-01T08:19:46Z
  file_id: '20717'
  file_name: 2025_PhysReviewLetters_Stoellner.pdf
  file_size: 1761373
  relation: main_file
  success: 1
file_date_updated: 2025-12-01T08:19:46Z
has_accepted_license: '1'
intvolume: '       135'
issue: '21'
language:
- iso: eng
month: '11'
oa: 1
oa_version: Published Version
project:
- _id: 0aa60e99-070f-11eb-9043-a6de6bdc3afa
  call_identifier: H2020
  grant_number: '949120'
  name: 'Tribocharge: a multi-scale approach to an enduring problem in physics'
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Physical Review Letters
publication_identifier:
  eissn:
  - 1079-7114
  issn:
  - 0031-9007
publication_status: published
publisher: American Physical Society
quality_controlled: '1'
related_material:
  link:
  - description: News on ISTA website
    relation: press_release
    url: https://ista.ac.at/en/news/trapping-particles-to-explain-lightning/
scopus_import: '1'
status: public
title: Using optical tweezers to simultaneously trap, charge, and measure the charge
  of a microparticle in air
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: journal_article
user_id: ba8df636-2132-11f1-aed0-ed93e2281fdd
volume: 135
year: '2025'
...
---
APC_amount: 5651,35 EUR
OA_place: publisher
OA_type: hybrid
PlanS_conform: '1'
_id: '20795'
abstract:
- lang: eng
  text: The tropical climate variability is characterized by various oscillations
    across a range of timescales. Oscillations that imprint the tropical mean state
    are generally attributed to slow processes, such as the seasonal cycle or interannual
    variability. Here, we identify a pronounced tropics-wide intraseasonal oscillation
    (TWISO) in satellite observations and reanalyses. This oscillation, with a period
    of 30 to 60 d, is evident across multiple variables and involves interactions
    between convection, radiation, surface fluxes, and large-scale circulation. It
    is primarily manifested as convective perturbations in the tropical Indo-Pacific
    warm pool accompanied by oscillations in the large-scale tropical overturning
    circulation. Here, we examine the relationship between TWISO, the Madden–Julian
    Oscillation (MJO), and the instability of radiative-convective equilibrium. Certain
    phases of TWISO coincide with specific phases of the MJO, suggesting a potential
    connection between the two. However, although the MJO can amplify the oscillation
    amplitude of TWISO, it is not essential for TWISO to occur. Finally, due to its
    broad manifestation across the tropics, TWISO potentially exerts widespread influence
    on tropical weather and climate at regional scales.
acknowledgement: 'J.B. acknowledges funding from the European Union’s Horizon 2020
  research and innovation programme under the Marie Skłodowska-Curie grant (grant
  agreement No. 101034413). S.B. acknowledges funding from the European Research Council
  (ERC) under the European Union’s Horizon 2020 research and innovation program (Project
  Mesoscale organization of tropical convection, grant agreement No 101098063). D.T.
  acknowledges funding from the Japan Society for the Promotion of Science (JSPS)
  (Project JSPS Grants-in-Aid for Scientiﬁc Research, grant No. JP24K22893). C.M.
  gratefully acknowledges funding from the ERC under the European Union’s Horizon
  2020 research and innovation program (Project organisation of CLoUdS, and implications
  for Tropical cyclones and for the Energetics of the tropics, in current and in a
  waRming climate, grant agreement No. 805041). We thank Martin Singh, Steven Sherwood,
  Bjorn Stevens, and Lokahith Agasthya for helpful discussions. JSPS Core-to-Core
  Program, “International Core-to-Core Project on Global Storm Resolving Analysis”
  (Grant Number: JPJSCCA20220001)'
article_number: e2511549122
article_processing_charge: Yes (in subscription journal)
article_type: original
author:
- first_name: Jiawei
  full_name: Bao, Jiawei
  id: bb9a7399-fefd-11ed-be3c-ae648fd1d160
  last_name: Bao
- first_name: Sandrine
  full_name: Bony, Sandrine
  last_name: Bony
- first_name: Daisuke
  full_name: Takasuka, Daisuke
  last_name: Takasuka
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
citation:
  ama: Bao J, Bony S, Takasuka D, Muller CJ. Tropics-wide intraseasonal oscillations.
    <i>Proceedings of the National Academy of Sciences</i>. 2025;122(48). doi:<a href="https://doi.org/10.1073/pnas.2511549122">10.1073/pnas.2511549122</a>
  apa: Bao, J., Bony, S., Takasuka, D., &#38; Muller, C. J. (2025). Tropics-wide intraseasonal
    oscillations. <i>Proceedings of the National Academy of Sciences</i>. National
    Academy of Sciences. <a href="https://doi.org/10.1073/pnas.2511549122">https://doi.org/10.1073/pnas.2511549122</a>
  chicago: Bao, Jiawei, Sandrine Bony, Daisuke Takasuka, and Caroline J Muller. “Tropics-Wide
    Intraseasonal Oscillations.” <i>Proceedings of the National Academy of Sciences</i>.
    National Academy of Sciences, 2025. <a href="https://doi.org/10.1073/pnas.2511549122">https://doi.org/10.1073/pnas.2511549122</a>.
  ieee: J. Bao, S. Bony, D. Takasuka, and C. J. Muller, “Tropics-wide intraseasonal
    oscillations,” <i>Proceedings of the National Academy of Sciences</i>, vol. 122,
    no. 48. National Academy of Sciences, 2025.
  ista: Bao J, Bony S, Takasuka D, Muller CJ. 2025. Tropics-wide intraseasonal oscillations.
    Proceedings of the National Academy of Sciences. 122(48), e2511549122.
  mla: Bao, Jiawei, et al. “Tropics-Wide Intraseasonal Oscillations.” <i>Proceedings
    of the National Academy of Sciences</i>, vol. 122, no. 48, e2511549122, National
    Academy of Sciences, 2025, doi:<a href="https://doi.org/10.1073/pnas.2511549122">10.1073/pnas.2511549122</a>.
  short: J. Bao, S. Bony, D. Takasuka, C.J. Muller, Proceedings of the National Academy
    of Sciences 122 (2025).
corr_author: '1'
date_created: 2025-12-11T10:41:13Z
date_published: 2025-12-02T00:00:00Z
date_updated: 2026-05-20T08:11:56Z
day: '02'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1073/pnas.2511549122
ec_funded: 1
external_id:
  pmid:
  - '41284872'
file:
- access_level: open_access
  checksum: 093a8685170e4a1de9176f68ee449493
  content_type: application/pdf
  creator: dernst
  date_created: 2025-12-15T09:17:33Z
  date_updated: 2025-12-15T09:17:33Z
  file_id: '20822'
  file_name: 2025_PNAS_Bao.pdf
  file_size: 30890293
  relation: main_file
  success: 1
file_date_updated: 2025-12-15T09:17:33Z
has_accepted_license: '1'
intvolume: '       122'
issue: '48'
language:
- iso: eng
month: '12'
oa: 1
oa_version: Published Version
pmid: 1
project:
- _id: fc2ed2f7-9c52-11eb-aca3-c01059dda49c
  call_identifier: H2020
  grant_number: '101034413'
  name: 'IST-BRIDGE: International postdoctoral program'
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Proceedings of the National Academy of Sciences
publication_identifier:
  eissn:
  - 1091-6490
  issn:
  - 0027-8424
publication_status: published
publisher: National Academy of Sciences
quality_controlled: '1'
related_material:
  link:
  - description: News on ISTA website
    relation: press_release
    url: https://ista.ac.at/en/news/hidden-in-plain-sight/
scopus_import: '1'
status: public
title: Tropics-wide intraseasonal oscillations
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 122
year: '2025'
...
---
APC_amount: 3774 EUR
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '20026'
abstract:
- lang: eng
  text: Deep Convective Systems (DCSs) reaching scales of 100–1000 km play a pivotal
    role as the primary precipitation source in the tropics. Those systems can have
    large cloud shields, and thus not only affect severe precipitation patterns but
    also play a crucial part in modulating the tropical radiation budget. Understanding
    the complex factors that control how these systems grow and how they will behave
    in a warming climate remain fundamental challenges. Research efforts have been
    directed, on one hand, towards understanding the environmental control on these
    systems, and on the other hand, towards exploring the internal potential of systems
    to develop and self-aggregate in idealized simulations. However, we still lack
    understanding on the relative role of the environment and internal feedbacks on
    DCS mature size and why. The novel high-resolution global SAM simulation from
    the DYAMOND project, combined with the TOOCAN Lagrangian tracking of DCSs and
    machine learning tools, offers an unprecedented opportunity to explore this question.
    We find that a system’s growth rate during the first 2 h of development predicts
    its final size with a Pearson correlation coefficient of 0.65. Beyond this period,
    growth rate emerges as the strongest predictor. However, in the early stages,
    additional factors–such as ice water path heterogeneity, migration distance, interactions
    with neighboring systems, and deep shear–play a more significant role. Our study
    quantitatively assesses the relative influence of internal versus external factors
    on the mature cloud shield size. Our results show that system-intrinsic properties
    exert a stronger influence than environmental conditions, suggesting that the
    initial environment does not strictly constrain final system size, particularly
    for larger systems where internal dynamics dominate.
acknowledgement: C.M. and S.A. gratefully acknowledge funding from the European Research
  Council (ERC) under the European Union's Horizon 2020 research and innovation program
  (Project CLUSTER, grant agreement 805041), and from the PhD fellowship of Ecole
  Normale Supérieure de Paris-Saclay. DYAMOND data management was provided by the
  German Climate Computing Center (DKRZ) and supported through the projects ESiWACE
  and ESiWACE2. The projects ESiWACE and ESiWACE2 have received funding from the European
  Union’s Horizon 2020 research and innovation program under grant agreements No 675191
  and 823988. This work used resources of the Deutsches Klimarechenzentrum (DKRZ)
  granted by its Scientific Steering Committee (WLA) under project IDs bk1040 and
  bb1153. The authors express their gratitude to Sophie Cloché and Eileen Hertwig
  for their assistance in data archival at IPSL and DKRZ, respectively. We also thank
  Christophe Lampert and Benjamin Fildier for valuable scientific discussions, and
  acknowledge the thoughtful comments of two anonymous reviewers.
article_number: '258'
article_processing_charge: Yes
article_type: original
author:
- first_name: Sophie
  full_name: Abramian, Sophie
  last_name: Abramian
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
- first_name: Camille
  full_name: Risi, Camille
  last_name: Risi
- first_name: Thomas
  full_name: Fiolleau, Thomas
  last_name: Fiolleau
- first_name: Rémy
  full_name: Roca, Rémy
  last_name: Roca
citation:
  ama: Abramian S, Muller CJ, Risi C, Fiolleau T, Roca R. How key features of early
    development shape deep convective systems. <i>npj Climate and Atmospheric Science</i>.
    2025;8. doi:<a href="https://doi.org/10.1038/s41612-025-01154-1">10.1038/s41612-025-01154-1</a>
  apa: Abramian, S., Muller, C. J., Risi, C., Fiolleau, T., &#38; Roca, R. (2025).
    How key features of early development shape deep convective systems. <i>Npj Climate
    and Atmospheric Science</i>. Springer Nature. <a href="https://doi.org/10.1038/s41612-025-01154-1">https://doi.org/10.1038/s41612-025-01154-1</a>
  chicago: Abramian, Sophie, Caroline J Muller, Camille Risi, Thomas Fiolleau, and
    Rémy Roca. “How Key Features of Early Development Shape Deep Convective Systems.”
    <i>Npj Climate and Atmospheric Science</i>. Springer Nature, 2025. <a href="https://doi.org/10.1038/s41612-025-01154-1">https://doi.org/10.1038/s41612-025-01154-1</a>.
  ieee: S. Abramian, C. J. Muller, C. Risi, T. Fiolleau, and R. Roca, “How key features
    of early development shape deep convective systems,” <i>npj Climate and Atmospheric
    Science</i>, vol. 8. Springer Nature, 2025.
  ista: Abramian S, Muller CJ, Risi C, Fiolleau T, Roca R. 2025. How key features
    of early development shape deep convective systems. npj Climate and Atmospheric
    Science. 8, 258.
  mla: Abramian, Sophie, et al. “How Key Features of Early Development Shape Deep
    Convective Systems.” <i>Npj Climate and Atmospheric Science</i>, vol. 8, 258,
    Springer Nature, 2025, doi:<a href="https://doi.org/10.1038/s41612-025-01154-1">10.1038/s41612-025-01154-1</a>.
  short: S. Abramian, C.J. Muller, C. Risi, T. Fiolleau, R. Roca, Npj Climate and
    Atmospheric Science 8 (2025).
date_created: 2025-07-20T22:01:59Z
date_published: 2025-07-08T00:00:00Z
date_updated: 2026-05-20T08:39:39Z
day: '08'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1038/s41612-025-01154-1
ec_funded: 1
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month: '07'
oa: 1
oa_version: Published Version
project:
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: npj Climate and Atmospheric Science
publication_identifier:
  eissn:
  - 2397-3722
publication_status: published
publisher: Springer Nature
quality_controlled: '1'
scopus_import: '1'
status: public
title: How key features of early development shape deep convective systems
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  short: CC BY-NC-ND (4.0)
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
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year: '2025'
...
---
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '18708'
abstract:
- lang: eng
  text: This study investigates the response of Indian summer monsoon (ISM) precipitation
    to CO2 removal, with a specific focus on regional and subseasonal variations.
    Following CO2 removal, monsoon circulation weakens throughout the summer owing
    to the reduced large-scale meridional temperature gradient around India. Weakened
    monsoon circulation decreases the local-scale thermodynamic stability within India,
    following monsoon-onset periods. While the frequency of synoptic-scale ISM low-pressure
    systems (LPSs) decreases overall, the lower thermodynamic stability causes the
    LPSs to form and resultantly shift west and south from their typical paths, last
    longer and move more quickly zonally during August and September. Changes in these
    rain-producing processes induce distinct regional (Western Ghats, south-central-east
    India, and Tamil Nadu) and subseasonal precipitation responses. Also, extreme
    precipitation exhibits similar patterns, but is more strongly affected by changes
    in LPS. Our results suggest that reliable future projections of regional hydroclimate
    change require a more accurate understanding of multi-scale precipitation processes.
acknowledgement: This study was supported by the National Research Foundation of Korea
  (NRF) grant funded by the Korean government (MSIT) (NRF-2018R1A5A1024958, NRF-2021R1C1C2094185,
  RS-2024-00336160). Model simulation and data transfer were supported by the National
  Supercomputing Center with supercomputing resources including technical support
  (KSC-2021-CHA-0030), the National Center for Meteorological Supercomputer of the
  Korea Meteorological Administration (KMA), and by the Korea Research Environment
  Open NETwork (KREONET), respectively. DK was supported by New Faculty Startup Fund
  from Seoul National University. We acknowledge the World Climate Research Programme,
  which, through its Working Group on Coupled Modelling, coordinated and promoted
  CMIP6. We thank the climate modeling groups for producing and making available their
  model output, the Earth System Grid Federation (ESGF) for archiving the data and
  providing access (https://esgf-node.llnl.gov/projects/cmip6/), and the multiple
  funding agencies who support CMIP6 and ESGF.
article_number: '305'
article_processing_charge: Yes
article_type: original
author:
- first_name: Seungmok
  full_name: Paik, Seungmok
  last_name: Paik
- first_name: Daehyun
  full_name: Kim, Daehyun
  last_name: Kim
- first_name: Soon Il
  full_name: An, Soon Il
  last_name: An
- first_name: Hyoeun
  full_name: Oh, Hyoeun
  last_name: Oh
- first_name: Jongsoo
  full_name: Shin, Jongsoo
  last_name: Shin
- first_name: Bidyut B
  full_name: Goswami, Bidyut B
  id: 3a4ac09c-6d61-11ec-bf66-884cde66b64b
  last_name: Goswami
  orcid: 0000-0001-8602-3083
- first_name: Seung Ki
  full_name: Min, Seung Ki
  last_name: Min
- first_name: Sanjit Kumar
  full_name: Mondal, Sanjit Kumar
  last_name: Mondal
citation:
  ama: Paik S, Kim D, An SI, et al. Exploring causes of distinct regional and subseasonal
    Indian summer monsoon precipitation responses to CO2 removal. <i>npj Climate and
    Atmospheric Science</i>. 2024;7. doi:<a href="https://doi.org/10.1038/s41612-024-00858-0">10.1038/s41612-024-00858-0</a>
  apa: Paik, S., Kim, D., An, S. I., Oh, H., Shin, J., GOSWAMI, B. B., … Mondal, S.
    K. (2024). Exploring causes of distinct regional and subseasonal Indian summer
    monsoon precipitation responses to CO2 removal. <i>Npj Climate and Atmospheric
    Science</i>. Springer Nature. <a href="https://doi.org/10.1038/s41612-024-00858-0">https://doi.org/10.1038/s41612-024-00858-0</a>
  chicago: Paik, Seungmok, Daehyun Kim, Soon Il An, Hyoeun Oh, Jongsoo Shin, BIDYUT
    B GOSWAMI, Seung Ki Min, and Sanjit Kumar Mondal. “Exploring Causes of Distinct
    Regional and Subseasonal Indian Summer Monsoon Precipitation Responses to CO2
    Removal.” <i>Npj Climate and Atmospheric Science</i>. Springer Nature, 2024. <a
    href="https://doi.org/10.1038/s41612-024-00858-0">https://doi.org/10.1038/s41612-024-00858-0</a>.
  ieee: S. Paik <i>et al.</i>, “Exploring causes of distinct regional and subseasonal
    Indian summer monsoon precipitation responses to CO2 removal,” <i>npj Climate
    and Atmospheric Science</i>, vol. 7. Springer Nature, 2024.
  ista: Paik S, Kim D, An SI, Oh H, Shin J, GOSWAMI BB, Min SK, Mondal SK. 2024. Exploring
    causes of distinct regional and subseasonal Indian summer monsoon precipitation
    responses to CO2 removal. npj Climate and Atmospheric Science. 7, 305.
  mla: Paik, Seungmok, et al. “Exploring Causes of Distinct Regional and Subseasonal
    Indian Summer Monsoon Precipitation Responses to CO2 Removal.” <i>Npj Climate
    and Atmospheric Science</i>, vol. 7, 305, Springer Nature, 2024, doi:<a href="https://doi.org/10.1038/s41612-024-00858-0">10.1038/s41612-024-00858-0</a>.
  short: S. Paik, D. Kim, S.I. An, H. Oh, J. Shin, B.B. GOSWAMI, S.K. Min, S.K. Mondal,
    Npj Climate and Atmospheric Science 7 (2024).
date_created: 2024-12-29T23:01:57Z
date_published: 2024-12-19T00:00:00Z
date_updated: 2025-09-09T11:51:56Z
day: '19'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1038/s41612-024-00858-0
external_id:
  isi:
  - '001381218300007'
file:
- access_level: open_access
  checksum: 6b3148315a444835113c32b399010370
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has_accepted_license: '1'
intvolume: '         7'
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language:
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month: '12'
oa: 1
oa_version: Published Version
publication: npj Climate and Atmospheric Science
publication_identifier:
  eissn:
  - 2397-3722
publication_status: published
publisher: Springer Nature
quality_controlled: '1'
scopus_import: '1'
status: public
title: Exploring causes of distinct regional and subseasonal Indian summer monsoon
  precipitation responses to CO2 removal
tmp:
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  short: CC BY-NC-ND (4.0)
type: journal_article
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volume: 7
year: '2024'
...
---
OA_place: publisher
OA_type: gold
_id: '19005'
abstract:
- lang: eng
  text: "Causal representation learning promises to extend causal models to hidden
    causal\r\nvariables from raw entangled measurements. However, most progress has
    focused\r\non proving identifiability results in different settings, and we are
    not aware of any\r\nsuccessful real-world application. At the same time, the field
    of dynamical systems\r\nbenefited from deep learning and scaled to countless applications
    but does not allow\r\nparameter identification. In this paper, we draw a clear
    connection between the two\r\nand their key assumptions, allowing us to apply
    identifiable methods developed\r\nin causal representation learning to dynamical
    systems. At the same time, we can\r\nleverage scalable differentiable solvers
    developed for differential equations to build\r\nmodels that are both identifiable
    and practical. Overall, we learn explicitly controllable models that isolate the
    trajectory-specific parameters for further downstream\r\ntasks such as out-of-distribution
    classification or treatment effect estimation. We\r\nexperiment with a wind simulator
    with partially known factors of variation. We\r\nalso apply the resulting model
    to real-world climate data and successfully answer\r\ndownstream causal questions
    in line with existing literature on climate change.\r\nCode is available at https://github.com/CausalLearningAI/crl-dynamical-systems."
acknowledgement: "We thank Niklas Boers for recommending the SpeedyWeather simulator
  and Valentino Maiorca\r\nfor guidance on Fourier transformation for SST data. We
  are also grateful to Shimeng Huang and Riccardo Cadei for their feedback on the
  treatment effect estimation experiment and to Jiale Chen and Adeel Pervez for their
  assistance with the solver implementation. Finally, we appreciate the anonymous
  reviewers for their insightful suggestions, which helped improve the manuscript. "
alternative_title:
- Advances in Neural Information Processing Systems
article_processing_charge: No
arxiv: 1
author:
- first_name: Dingling
  full_name: Yao, Dingling
  id: d3e02e50-48a8-11ee-8f62-c108061797fa
  last_name: Yao
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
- first_name: Francesco
  full_name: Locatello, Francesco
  id: 26cfd52f-2483-11ee-8040-88983bcc06d4
  last_name: Locatello
  orcid: 0000-0002-4850-0683
citation:
  ama: 'Yao D, Muller CJ, Locatello F. Marrying causal representation learning with
    dynamical systems for science. In: <i>38th Conference on Neural Information Processing
    Systems</i>. Vol 37. Neural Information Processing Systems Foundation; 2024.'
  apa: 'Yao, D., Muller, C. J., &#38; Locatello, F. (2024). Marrying causal representation
    learning with dynamical systems for science. In <i>38th Conference on Neural Information
    Processing Systems</i> (Vol. 37). Vancouver, Canada: Neural Information Processing
    Systems Foundation.'
  chicago: Yao, Dingling, Caroline J Muller, and Francesco Locatello. “Marrying Causal
    Representation Learning with Dynamical Systems for Science.” In <i>38th Conference
    on Neural Information Processing Systems</i>, Vol. 37. Neural Information Processing
    Systems Foundation, 2024.
  ieee: D. Yao, C. J. Muller, and F. Locatello, “Marrying causal representation learning
    with dynamical systems for science,” in <i>38th Conference on Neural Information
    Processing Systems</i>, Vancouver, Canada, 2024, vol. 37.
  ista: 'Yao D, Muller CJ, Locatello F. 2024. Marrying causal representation learning
    with dynamical systems for science. 38th Conference on Neural Information Processing
    Systems. NeurIPS: Neural Information Processing Systems, Advances in Neural Information
    Processing Systems, vol. 37.'
  mla: Yao, Dingling, et al. “Marrying Causal Representation Learning with Dynamical
    Systems for Science.” <i>38th Conference on Neural Information Processing Systems</i>,
    vol. 37, Neural Information Processing Systems Foundation, 2024.
  short: D. Yao, C.J. Muller, F. Locatello, in:, 38th Conference on Neural Information
    Processing Systems, Neural Information Processing Systems Foundation, 2024.
conference:
  end_date: 2024-12-16
  location: Vancouver, Canada
  name: 'NeurIPS: Neural Information Processing Systems'
  start_date: 2024-12-16
corr_author: '1'
date_created: 2025-02-05T07:49:00Z
date_published: 2024-12-01T00:00:00Z
date_updated: 2025-07-10T11:51:32Z
day: '01'
ddc:
- '000'
- '550'
department:
- _id: CaMu
- _id: FrLo
external_id:
  arxiv:
  - '2405.13888'
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  file_id: '19006'
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has_accepted_license: '1'
intvolume: '        37'
language:
- iso: eng
month: '12'
oa: 1
oa_version: Published Version
publication: 38th Conference on Neural Information Processing Systems
publication_status: published
publisher: Neural Information Processing Systems Foundation
quality_controlled: '1'
related_material:
  link:
  - relation: software
    url: https://github.com/CausalLearningAI/crl-dynamical-systems
scopus_import: '1'
status: public
title: Marrying causal representation learning with dynamical systems for science
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: conference
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 37
year: '2024'
...
---
OA_place: repository
OA_type: green
_id: '19307'
abstract:
- lang: eng
  text: "This repository contains the data, scripts, SAM codes and files required
    to reproduce the results of the manuscript \"The Unreasonable Efficiency of Total
    Rain Evaporation Removal in Triggering Convective Self-Aggregation\" submitted
    to the Geophysical Research Letters (GRL).\r\n\r\nBrief description of project:
    This project aims to examine the impact of rain evaporation removal or reduction
    in the planetary boundary layer (PBL) on convective self aggregation (CSA). Non-rotating
    radiative-convective equilibrium (RCE) simulations were conducted with the System
    for Atmospheric Modeling (SAM) cloud resolving model. Rain evaporation in the
    lowest 1 km was progressively reduced and the effect on CSA was investigated.
    The physical processes underlying this type of aggregation (referred to in the
    manuscript as no-evaporation CSA, or NE-CSA) were analyzed and described. \r\nThe
    default SAM code base (version 6.10.8) can be downloaded from here: http://rossby.msrc.sunysb.edu/~marat/SAM.html"
article_processing_charge: No
author:
- first_name: Yi-Ling
  full_name: Hwong, Yi-Ling
  id: 1217aa61-4dd1-11ec-9ac3-f2ba3f17ee22
  last_name: Hwong
  orcid: 0000-0001-9281-3479
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
citation:
  ama: Hwong Y-L, Muller CJ. Data - The unreasonable efficiency of total rain evaporation
    removal in triggering convective self-aggregation. 2024. doi:<a href="https://doi.org/10.5281/ZENODO.10687169">10.5281/ZENODO.10687169</a>
  apa: Hwong, Y.-L., &#38; Muller, C. J. (2024). Data - The unreasonable efficiency
    of total rain evaporation removal in triggering convective self-aggregation. Zenodo.
    <a href="https://doi.org/10.5281/ZENODO.10687169">https://doi.org/10.5281/ZENODO.10687169</a>
  chicago: Hwong, Yi-Ling, and Caroline J Muller. “Data - The Unreasonable Efficiency
    of Total Rain Evaporation Removal in Triggering Convective Self-Aggregation.”
    Zenodo, 2024. <a href="https://doi.org/10.5281/ZENODO.10687169">https://doi.org/10.5281/ZENODO.10687169</a>.
  ieee: Y.-L. Hwong and C. J. Muller, “Data - The unreasonable efficiency of total
    rain evaporation removal in triggering convective self-aggregation.” Zenodo, 2024.
  ista: Hwong Y-L, Muller CJ. 2024. Data - The unreasonable efficiency of total rain
    evaporation removal in triggering convective self-aggregation, Zenodo, <a href="https://doi.org/10.5281/ZENODO.10687169">10.5281/ZENODO.10687169</a>.
  mla: Hwong, Yi-Ling, and Caroline J. Muller. <i>Data - The Unreasonable Efficiency
    of Total Rain Evaporation Removal in Triggering Convective Self-Aggregation</i>.
    Zenodo, 2024, doi:<a href="https://doi.org/10.5281/ZENODO.10687169">10.5281/ZENODO.10687169</a>.
  short: Y.-L. Hwong, C.J. Muller, (2024).
corr_author: '1'
date_created: 2025-03-07T08:39:40Z
date_published: 2024-02-21T00:00:00Z
date_updated: 2025-09-04T13:16:39Z
day: '21'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.5281/ZENODO.10687169
has_accepted_license: '1'
main_file_link:
- open_access: '1'
  url: https://doi.org/10.5281/zenodo.8369509
month: '02'
oa: 1
oa_version: Published Version
publisher: Zenodo
related_material:
  record:
  - id: '15186'
    relation: used_in_publication
    status: public
status: public
title: Data - The unreasonable efficiency of total rain evaporation removal in triggering
  convective self-aggregation
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: research_data_reference
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
year: '2024'
...
---
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '15047'
abstract:
- lang: eng
  text: Tropical precipitation extremes and their changes with surface warming are
    investigated using global storm resolving simulations and high-resolution observations.
    The simulations demonstrate that the mesoscale organization of convection, a process
    that cannot be physically represented by conventional global climate models, is
    important for the variations of tropical daily accumulated precipitation extremes.
    In both the simulations and observations, daily precipitation extremes increase
    in a more organized state, in association with larger, but less frequent, storms.
    Repeating the simulations for a warmer climate results in a robust increase in
    monthly-mean daily precipitation extremes. Higher precipitation percentiles have
    a greater sensitivity to convective organization, which is predicted to increase
    with warming. Without changes in organization, the strongest daily precipitation
    extremes over the tropical oceans increase at a rate close to Clausius-Clapeyron
    (CC) scaling. Thus, in a future warmer state with increased organization, the
    strongest daily precipitation extremes over oceans increase at a faster rate than
    CC scaling.
acknowledgement: This work is supported by the Max-Planck-Gesellschaft (MPG). We greatly
  appreciate computational resources from Deutsches Klimarechenzentrum (DKRZ) and
  the Jülich Supercomputing Centre (JSC). ICONA/O simulations are funded through the
  NextGEMS project by the EU’s Horizon 2020 programme (grant agreement no. 101003470).
  ICONA simulations are funded through the MONSOON-2.0 project (grant agreement no.
  01LP1927A) which is supported from German Federal Ministry of Education and Research
  (BMBF). J.B. acknowledges funding from the European Union’s Horizon 2020 research
  and innovation programme under the Marie Skłodowska-Curie grant (grant agreement
  no. 101034413). B.S. acknowledges funding from the EU’s Horizon 2020 programme (grant
  agreement no. 101003470). C.M. gratefully acknowledges funding from the European
  Research Council (ERC) under the European Union’s Horizon 2020 research and innovation
  program (Project CLUSTER, grant agreement no. 805041).
article_number: eadj6801
article_processing_charge: Yes
article_type: original
author:
- first_name: Jiawei
  full_name: Bao, Jiawei
  id: bb9a7399-fefd-11ed-be3c-ae648fd1d160
  last_name: Bao
- first_name: Bjorn
  full_name: Stevens, Bjorn
  last_name: Stevens
- first_name: Lukas
  full_name: Kluft, Lukas
  last_name: Kluft
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
citation:
  ama: Bao J, Stevens B, Kluft L, Muller CJ. Intensification of daily tropical precipitation
    extremes from more organized convection. <i>Science Advances</i>. 2024;10(8).
    doi:<a href="https://doi.org/10.1126/sciadv.adj6801">10.1126/sciadv.adj6801</a>
  apa: Bao, J., Stevens, B., Kluft, L., &#38; Muller, C. J. (2024). Intensification
    of daily tropical precipitation extremes from more organized convection. <i>Science
    Advances</i>. American Association for the Advancement of Science. <a href="https://doi.org/10.1126/sciadv.adj6801">https://doi.org/10.1126/sciadv.adj6801</a>
  chicago: Bao, Jiawei, Bjorn Stevens, Lukas Kluft, and Caroline J Muller. “Intensification
    of Daily Tropical Precipitation Extremes from More Organized Convection.” <i>Science
    Advances</i>. American Association for the Advancement of Science, 2024. <a href="https://doi.org/10.1126/sciadv.adj6801">https://doi.org/10.1126/sciadv.adj6801</a>.
  ieee: J. Bao, B. Stevens, L. Kluft, and C. J. Muller, “Intensification of daily
    tropical precipitation extremes from more organized convection,” <i>Science Advances</i>,
    vol. 10, no. 8. American Association for the Advancement of Science, 2024.
  ista: Bao J, Stevens B, Kluft L, Muller CJ. 2024. Intensification of daily tropical
    precipitation extremes from more organized convection. Science Advances. 10(8),
    eadj6801.
  mla: Bao, Jiawei, et al. “Intensification of Daily Tropical Precipitation Extremes
    from More Organized Convection.” <i>Science Advances</i>, vol. 10, no. 8, eadj6801,
    American Association for the Advancement of Science, 2024, doi:<a href="https://doi.org/10.1126/sciadv.adj6801">10.1126/sciadv.adj6801</a>.
  short: J. Bao, B. Stevens, L. Kluft, C.J. Muller, Science Advances 10 (2024).
date_created: 2024-03-03T23:00:50Z
date_published: 2024-02-23T00:00:00Z
date_updated: 2025-09-04T12:11:18Z
day: '23'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1126/sciadv.adj6801
ec_funded: 1
external_id:
  isi:
  - '001300045100007'
  pmid:
  - '38394192'
file:
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has_accepted_license: '1'
intvolume: '        10'
isi: 1
issue: '8'
language:
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month: '02'
oa: 1
oa_version: Published Version
pmid: 1
project:
- _id: fc2ed2f7-9c52-11eb-aca3-c01059dda49c
  call_identifier: H2020
  grant_number: '101034413'
  name: 'IST-BRIDGE: International postdoctoral program'
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Science Advances
publication_identifier:
  eissn:
  - 2375-2548
publication_status: published
publisher: American Association for the Advancement of Science
quality_controlled: '1'
related_material:
  link:
  - description: News on ISTA Website
    relation: press_release
    url: https://ista.ac.at/en/news/cloud-clustering-causes-more-extreme-rain/
scopus_import: '1'
status: public
title: Intensification of daily tropical precipitation extremes from more organized
  convection
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: journal_article
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volume: 10
year: '2024'
...
---
_id: '15097'
abstract:
- lang: eng
  text: Global storm-resolving models (GSRMs) use strongly refined horizontal grids
    compared with the climate models typically used in the Coupled Model Intercomparison
    Project (CMIP) but employ comparable vertical grid spacings. Here, we study how
    changes in the vertical grid spacing and adjustments to the integration time step
    affect the basic climate quantities simulated by the ICON-Sapphire atmospheric
    GSRM. Simulations are performed over a 45 d period for five different vertical
    grids with between 55 and 540 vertical layers and maximum tropospheric vertical
    grid spacings of between 800 and 50 m, respectively. The effects of changes in
    the vertical grid spacing are compared with the effects of reducing the horizontal
    grid spacing from 5 to 2.5 km. For most of the quantities considered, halving
    the vertical grid spacing has a smaller effect than halving the horizontal grid
    spacing, but it is not negligible. Each halving of the vertical grid spacing,
    along with the necessary reductions in time step length, increases cloud liquid
    water by about 7 %, compared with an approximate 16 % decrease for halving the
    horizontal grid spacing. The effect is due to both the vertical grid refinement
    and the time step reduction. There is no tendency toward convergence in the range
    of grid spacings tested here. The cloud ice amount also increases with a refinement
    in the vertical grid, but it is hardly affected by the time step length and does
    show a tendency to converge. While the effect on shortwave radiation is globally
    dominated by the altered reflection due to the change in the cloud liquid water
    content, the effect on longwave radiation is more difficult to interpret because
    changes in the cloud ice concentration and cloud fraction are anticorrelated in
    some regions. The simulations show that using a maximum tropospheric vertical
    grid spacing larger than 400 m would increase the truncation error strongly. Computing
    time investments in a further vertical grid refinement can affect the truncation
    errors of GSRMs similarly to comparable investments in horizontal refinement,
    because halving the vertical grid spacing is generally cheaper than halving the
    horizontal grid spacing. However, convergence of boundary layer cloud properties
    cannot be expected, even for the smallest maximum tropospheric grid spacing of
    50 m used in this study.
acknowledgement: "The authors wish to thank Ann Kristin Naumann and three anonymous
  reviewers for very helpful comments on an earlier version of this paper. We are
  grateful to René Redler and Karl-Hermann Wieners for useful recommendations regarding
  running the simulations. We thank Luis Kornblueh for providing an external vertical
  grid generator and resolving the memory requirements for the very fine vertical
  grids. We acknowledge Hauke Schulz for providing the radiosonde data. The simulations
  were run at the German Climate Computing Center (DKRZ), and we thank the DKRZ staff
  for their support.\r\nHauke Schmidt and Diego Jimenez-de la Cuesta received financial
  support from the SOCTOC project within the framework of the ROMIC program, funded
  by the German Ministry of Education and Research (BMBF) (grant no. 01LG1903A).\r\nThe
  article processing charges for this open-access publication were covered by the
  Max Planck Society."
article_processing_charge: Yes (via OA deal)
article_type: original
author:
- first_name: Hauke
  full_name: Schmidt, Hauke
  last_name: Schmidt
- first_name: Sebastian
  full_name: Rast, Sebastian
  last_name: Rast
- first_name: Jiawei
  full_name: Bao, Jiawei
  id: bb9a7399-fefd-11ed-be3c-ae648fd1d160
  last_name: Bao
- first_name: Amrit
  full_name: Cassim, Amrit
  last_name: Cassim
- first_name: Shih Wei
  full_name: Fang, Shih Wei
  last_name: Fang
- first_name: Diego
  full_name: Jimenez-De La Cuesta, Diego
  last_name: Jimenez-De La Cuesta
- first_name: Paul
  full_name: Keil, Paul
  last_name: Keil
- first_name: Lukas
  full_name: Kluft, Lukas
  last_name: Kluft
- first_name: Clarissa
  full_name: Kroll, Clarissa
  last_name: Kroll
- first_name: Theresa
  full_name: Lang, Theresa
  last_name: Lang
- first_name: Ulrike
  full_name: Niemeier, Ulrike
  last_name: Niemeier
- first_name: Andrea
  full_name: Schneidereit, Andrea
  last_name: Schneidereit
- first_name: Andrew I.L.
  full_name: Williams, Andrew I.L.
  last_name: Williams
- first_name: Bjorn
  full_name: Stevens, Bjorn
  last_name: Stevens
citation:
  ama: Schmidt H, Rast S, Bao J, et al. Effects of vertical grid spacing on the climate
    simulated in the ICON-Sapphire global storm-resolving model. <i>Geoscientific
    Model Development</i>. 2024;17(4):1563-1584. doi:<a href="https://doi.org/10.5194/gmd-17-1563-2024">10.5194/gmd-17-1563-2024</a>
  apa: Schmidt, H., Rast, S., Bao, J., Cassim, A., Fang, S. W., Jimenez-De La Cuesta,
    D., … Stevens, B. (2024). Effects of vertical grid spacing on the climate simulated
    in the ICON-Sapphire global storm-resolving model. <i>Geoscientific Model Development</i>.
    European Geosciences Union. <a href="https://doi.org/10.5194/gmd-17-1563-2024">https://doi.org/10.5194/gmd-17-1563-2024</a>
  chicago: Schmidt, Hauke, Sebastian Rast, Jiawei Bao, Amrit Cassim, Shih Wei Fang,
    Diego Jimenez-De La Cuesta, Paul Keil, et al. “Effects of Vertical Grid Spacing
    on the Climate Simulated in the ICON-Sapphire Global Storm-Resolving Model.” <i>Geoscientific
    Model Development</i>. European Geosciences Union, 2024. <a href="https://doi.org/10.5194/gmd-17-1563-2024">https://doi.org/10.5194/gmd-17-1563-2024</a>.
  ieee: H. Schmidt <i>et al.</i>, “Effects of vertical grid spacing on the climate
    simulated in the ICON-Sapphire global storm-resolving model,” <i>Geoscientific
    Model Development</i>, vol. 17, no. 4. European Geosciences Union, pp. 1563–1584,
    2024.
  ista: Schmidt H, Rast S, Bao J, Cassim A, Fang SW, Jimenez-De La Cuesta D, Keil
    P, Kluft L, Kroll C, Lang T, Niemeier U, Schneidereit A, Williams AIL, Stevens
    B. 2024. Effects of vertical grid spacing on the climate simulated in the ICON-Sapphire
    global storm-resolving model. Geoscientific Model Development. 17(4), 1563–1584.
  mla: Schmidt, Hauke, et al. “Effects of Vertical Grid Spacing on the Climate Simulated
    in the ICON-Sapphire Global Storm-Resolving Model.” <i>Geoscientific Model Development</i>,
    vol. 17, no. 4, European Geosciences Union, 2024, pp. 1563–84, doi:<a href="https://doi.org/10.5194/gmd-17-1563-2024">10.5194/gmd-17-1563-2024</a>.
  short: H. Schmidt, S. Rast, J. Bao, A. Cassim, S.W. Fang, D. Jimenez-De La Cuesta,
    P. Keil, L. Kluft, C. Kroll, T. Lang, U. Niemeier, A. Schneidereit, A.I.L. Williams,
    B. Stevens, Geoscientific Model Development 17 (2024) 1563–1584.
date_created: 2024-03-10T23:00:53Z
date_published: 2024-02-22T00:00:00Z
date_updated: 2025-09-04T12:17:17Z
day: '22'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.5194/gmd-17-1563-2024
external_id:
  isi:
  - '001190535000001'
file:
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  date_created: 2024-03-13T08:59:21Z
  date_updated: 2024-03-13T08:59:21Z
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file_date_updated: 2024-03-13T08:59:21Z
has_accepted_license: '1'
intvolume: '        17'
isi: 1
issue: '4'
language:
- iso: eng
month: '02'
oa: 1
oa_version: Published Version
page: 1563-1584
publication: Geoscientific Model Development
publication_identifier:
  eissn:
  - 1991-9603
  issn:
  - 1991-959X
publication_status: published
publisher: European Geosciences Union
quality_controlled: '1'
scopus_import: '1'
status: public
title: Effects of vertical grid spacing on the climate simulated in the ICON-Sapphire
  global storm-resolving model
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 17
year: '2024'
...
---
APC_amount: 1470 EUR
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '15165'
abstract:
- lang: eng
  text: Current knowledge suggests a drought Indian monsoon (perhaps a severe one)
    when the El Nino Southern Oscillation and Pacific Decadal Oscillation each exhibit
    positive phases (a joint positive phase). For the monsoons, which are exceptions
    in this regard, we found northeast India often gets excess pre-monsoon rainfall.
    Further investigation reveals that this excess pre-monsoon rainfall is produced
    by the interaction of the large-scale circulation associated with the joint phase
    with the mountains in northeast India. We posit that a warmer troposphere, a consequence
    of excess rainfall over northeast India, drives a stronger monsoon circulation
    and enhances monsoon rainfall over central India. Hence, we argue that pre-monsoon
    rainfall over northeast India can be used for seasonal monsoon rainfall prediction
    over central India. Most importantly, its predictive value is at its peak when
    the Pacific Ocean exhibits a joint positive phase and the threat of extreme drought
    monsoon looms over India.
acknowledgement: The author gratefully acknowledges ISTA for supporting this research
  through funding from the European Research Council (ERC) under the European Union’s
  Horizon 2020 research and innovation programme (Project CLUSTER, grant agreement
  No. 805041).
article_number: e2023GL106569
article_processing_charge: Yes
article_type: original
author:
- first_name: Bidyut B
  full_name: Goswami, Bidyut B
  id: 3a4ac09c-6d61-11ec-bf66-884cde66b64b
  last_name: Goswami
  orcid: 0000-0001-8602-3083
citation:
  ama: GOSWAMI BB. A pre-monsoon signal of false alarms of Indian monsoon droughts.
    <i>Geophysical Research Letters</i>. 2024;51(5). doi:<a href="https://doi.org/10.1029/2023GL106569">10.1029/2023GL106569</a>
  apa: GOSWAMI, B. B. (2024). A pre-monsoon signal of false alarms of Indian monsoon
    droughts. <i>Geophysical Research Letters</i>. Wiley. <a href="https://doi.org/10.1029/2023GL106569">https://doi.org/10.1029/2023GL106569</a>
  chicago: GOSWAMI, BIDYUT B. “A Pre-Monsoon Signal of False Alarms of Indian Monsoon
    Droughts.” <i>Geophysical Research Letters</i>. Wiley, 2024. <a href="https://doi.org/10.1029/2023GL106569">https://doi.org/10.1029/2023GL106569</a>.
  ieee: B. B. GOSWAMI, “A pre-monsoon signal of false alarms of Indian monsoon droughts,”
    <i>Geophysical Research Letters</i>, vol. 51, no. 5. Wiley, 2024.
  ista: GOSWAMI BB. 2024. A pre-monsoon signal of false alarms of Indian monsoon droughts.
    Geophysical Research Letters. 51(5), e2023GL106569.
  mla: GOSWAMI, BIDYUT B. “A Pre-Monsoon Signal of False Alarms of Indian Monsoon
    Droughts.” <i>Geophysical Research Letters</i>, vol. 51, no. 5, e2023GL106569,
    Wiley, 2024, doi:<a href="https://doi.org/10.1029/2023GL106569">10.1029/2023GL106569</a>.
  short: B.B. GOSWAMI, Geophysical Research Letters 51 (2024).
corr_author: '1'
date_created: 2024-03-24T23:00:58Z
date_published: 2024-03-16T00:00:00Z
date_updated: 2025-09-04T13:11:41Z
day: '16'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2023GL106569
ec_funded: 1
external_id:
  isi:
  - '001181635700001'
file:
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  content_type: application/pdf
  creator: dernst
  date_created: 2024-03-25T08:36:00Z
  date_updated: 2024-03-25T08:36:00Z
  file_id: '15178'
  file_name: 2024_GeophysResLetters_Goswami.pdf
  file_size: 2887134
  relation: main_file
  success: 1
file_date_updated: 2024-03-25T08:36:00Z
has_accepted_license: '1'
intvolume: '        51'
isi: 1
issue: '5'
language:
- iso: eng
month: '03'
oa: 1
oa_version: Published Version
project:
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Geophysical Research Letters
publication_identifier:
  eissn:
  - 1944-8007
  issn:
  - 0094-8276
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: A pre-monsoon signal of false alarms of Indian monsoon droughts
tmp:
  image: /images/cc_by_nc_nd.png
  legal_code_url: https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
  name: Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
    (CC BY-NC-ND 4.0)
  short: CC BY-NC-ND (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 51
year: '2024'
...
---
APC_amount: 2940 EUR
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '15186'
abstract:
- lang: eng
  text: The elimination of rain evaporation in the planetary boundary layer (PBL)
    has been found to lead to convective self‐aggregation (CSA) even without radiative
    feedback, but the precise mechanisms underlying this phenomenon remain unclear.
    We conducted cloud‐resolving simulations with two domain sizes and progressively
    reduced rain evaporation in the PBL. Surprisingly, CSA only occurred when rain
    evaporation was almost completely removed. The additional convective heating resulting
    from the reduction of evaporative cooling in the moist patch was found to be the
    trigger, thereafter a dry subsidence intrusion into the PBL in the dry patch takes
    over and sets CSA in motion. Temperature and moisture anomalies oppose each other
    in their buoyancy effects, hence explaining the need for almost total rain evaporation
    removal. We also found radiative cooling and not cold pools to be the leading
    cause for the comparative ease of CSA to take place in the larger domain.
acknowledgement: "YLH is supported by funding from the European Union's Horizon 2020
  research and innovation programme under the Marie Skłodowska-Curie Grant 101034413.
  CM gratefully acknowledges funding from the European Research Council (ERC) under
  the European Union's Horizon 2020 research and innovation program (Project CLUSTER,
  Grant 805041). The authors warmly thank Steven Sherwood, Jiawei Bao, Bidyut Goswami,
  and Martin Janssens for stimulating and helpful discussions. They also thank Christopher
  Holloway and an anonymous reviewer for providing helpful feedback that greatly improved
  this manuscript.\r\n"
article_number: ' e2023GL106523'
article_processing_charge: Yes
article_type: original
author:
- first_name: Yi-Ling
  full_name: Hwong, Yi-Ling
  id: 1217aa61-4dd1-11ec-9ac3-f2ba3f17ee22
  last_name: Hwong
  orcid: 0000-0001-9281-3479
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
citation:
  ama: Hwong Y-L, Muller CJ. The unreasonable efficiency of total rain evaporation
    removal in triggering convective self‐aggregation. <i>Geophysical Research Letters</i>.
    2024;51(6). doi:<a href="https://doi.org/10.1029/2023gl106523">10.1029/2023gl106523</a>
  apa: Hwong, Y.-L., &#38; Muller, C. J. (2024). The unreasonable efficiency of total
    rain evaporation removal in triggering convective self‐aggregation. <i>Geophysical
    Research Letters</i>. Wiley. <a href="https://doi.org/10.1029/2023gl106523">https://doi.org/10.1029/2023gl106523</a>
  chicago: Hwong, Yi-Ling, and Caroline J Muller. “The Unreasonable Efficiency of
    Total Rain Evaporation Removal in Triggering Convective Self‐aggregation.” <i>Geophysical
    Research Letters</i>. Wiley, 2024. <a href="https://doi.org/10.1029/2023gl106523">https://doi.org/10.1029/2023gl106523</a>.
  ieee: Y.-L. Hwong and C. J. Muller, “The unreasonable efficiency of total rain evaporation
    removal in triggering convective self‐aggregation,” <i>Geophysical Research Letters</i>,
    vol. 51, no. 6. Wiley, 2024.
  ista: Hwong Y-L, Muller CJ. 2024. The unreasonable efficiency of total rain evaporation
    removal in triggering convective self‐aggregation. Geophysical Research Letters.
    51(6), e2023GL106523.
  mla: Hwong, Yi-Ling, and Caroline J. Muller. “The Unreasonable Efficiency of Total
    Rain Evaporation Removal in Triggering Convective Self‐aggregation.” <i>Geophysical
    Research Letters</i>, vol. 51, no. 6, e2023GL106523, Wiley, 2024, doi:<a href="https://doi.org/10.1029/2023gl106523">10.1029/2023gl106523</a>.
  short: Y.-L. Hwong, C.J. Muller, Geophysical Research Letters 51 (2024).
corr_author: '1'
date_created: 2024-03-25T10:27:30Z
date_published: 2024-03-19T00:00:00Z
date_updated: 2025-09-04T13:16:39Z
day: '19'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2023gl106523
ec_funded: 1
external_id:
  isi:
  - '001187002300001'
file:
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  checksum: eacb011091a503b9e7b748fef639ba4c
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  creator: dernst
  date_created: 2024-03-25T11:28:25Z
  date_updated: 2024-03-25T11:28:25Z
  file_id: '15187'
  file_name: 2024_GeophysResLetters_Hwong.pdf
  file_size: 1280108
  relation: main_file
  success: 1
file_date_updated: 2024-03-25T11:28:25Z
has_accepted_license: '1'
intvolume: '        51'
isi: 1
issue: '6'
keyword:
- General Earth and Planetary Sciences
- Geophysics
language:
- iso: eng
month: '03'
oa: 1
oa_version: Published Version
project:
- _id: fc2ed2f7-9c52-11eb-aca3-c01059dda49c
  call_identifier: H2020
  grant_number: '101034413'
  name: 'IST-BRIDGE: International postdoctoral program'
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Geophysical Research Letters
publication_identifier:
  eissn:
  - 1944-8007
  issn:
  - 0094-8276
publication_status: published
publisher: Wiley
quality_controlled: '1'
related_material:
  record:
  - id: '19307'
    relation: research_data
    status: public
scopus_import: '1'
status: public
title: The unreasonable efficiency of total rain evaporation removal in triggering
  convective self‐aggregation
tmp:
  image: /images/cc_by_nc_nd.png
  legal_code_url: https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
  name: Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
    (CC BY-NC-ND 4.0)
  short: CC BY-NC-ND (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 51
year: '2024'
...
---
OA_place: publisher
OA_type: hybrid
_id: '15313'
abstract:
- lang: eng
  text: Our goal is to investigate fundamental properties of the system of internally
    cooled convection. The system consists of an upward thermal flux at the lower
    boundary, a mean temperature lapse-rate and a constant cooling term in the bulk
    with the bulk cooling in thermal equilibrium with the input heat flux. This simple
    model represents idealised dry convection in the atmospheric boundary layer, where
    the cooling mimics the radiative cooling to space notably through longwave radiation.
    We perform linear stability analysis of the model for different values of the
    mean stratification to derive the critical forcing above which the fluid is convectively
    unstable to small perturbations. The dynamic behavior of the fluid system is described
    and the scaling of various important measured quantities such as the total vertical
    convective heat flux and the upward mass flux is measured. We introduce a lapse-rate
    dependent dimensionless Rayleigh-number Ray that determines the behavior of the
    system, finding that the convective heat-flux and mass-flux scale approximately
    as Ray0.5 and Ray0.7 respectively. The area-fraction of the domain that is occupied
    by upward and downward moving fluid and the skewness of the vertical velocity
    are studied to understand the asymmetry inherent in the system. We conclude with
    a short discussion on the relevance to atmospheric convection and the scope for
    further investigations of atmospheric convection using similar simplified approaches.
acknowledged_ssus:
- _id: ScienComp
acknowledgement: This project has received funding from the European Union’s Horizon
  2020 research and innovation programme under the Marie Sklodowska–Curie grant agreement
  No. 101034413. CM gratefully acknowledges funding from the European Research Council
  (ERC) under the European Union’s Horizon 2020 research and innovation program (Project
  CLUSTER, Grant Agreement No. 805041). This research was supported by the Scientific
  Service Units (SSU) of IST Austria through resources provided by Scientific Computing
  (SciComp).
article_number: '108011'
article_processing_charge: Yes (via OA deal)
article_type: original
arxiv: 1
author:
- first_name: Lokahith N
  full_name: Agasthya, Lokahith N
  id: cd100965-0804-11ed-9c55-f4878ff4e877
  last_name: Agasthya
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
citation:
  ama: Agasthya LN, Muller CJ. Dynamics and scaling of internally cooled convection.
    <i>Communications in Nonlinear Science and Numerical Simulation</i>. 2024;134.
    doi:<a href="https://doi.org/10.1016/j.cnsns.2024.108011">10.1016/j.cnsns.2024.108011</a>
  apa: Agasthya, L. N., &#38; Muller, C. J. (2024). Dynamics and scaling of internally
    cooled convection. <i>Communications in Nonlinear Science and Numerical Simulation</i>.
    Elsevier. <a href="https://doi.org/10.1016/j.cnsns.2024.108011">https://doi.org/10.1016/j.cnsns.2024.108011</a>
  chicago: Agasthya, Lokahith N, and Caroline J Muller. “Dynamics and Scaling of Internally
    Cooled Convection.” <i>Communications in Nonlinear Science and Numerical Simulation</i>.
    Elsevier, 2024. <a href="https://doi.org/10.1016/j.cnsns.2024.108011">https://doi.org/10.1016/j.cnsns.2024.108011</a>.
  ieee: L. N. Agasthya and C. J. Muller, “Dynamics and scaling of internally cooled
    convection,” <i>Communications in Nonlinear Science and Numerical Simulation</i>,
    vol. 134. Elsevier, 2024.
  ista: Agasthya LN, Muller CJ. 2024. Dynamics and scaling of internally cooled convection.
    Communications in Nonlinear Science and Numerical Simulation. 134, 108011.
  mla: Agasthya, Lokahith N., and Caroline J. Muller. “Dynamics and Scaling of Internally
    Cooled Convection.” <i>Communications in Nonlinear Science and Numerical Simulation</i>,
    vol. 134, 108011, Elsevier, 2024, doi:<a href="https://doi.org/10.1016/j.cnsns.2024.108011">10.1016/j.cnsns.2024.108011</a>.
  short: L.N. Agasthya, C.J. Muller, Communications in Nonlinear Science and Numerical
    Simulation 134 (2024).
corr_author: '1'
date_created: 2024-04-14T22:01:01Z
date_published: 2024-07-01T00:00:00Z
date_updated: 2025-09-04T13:37:48Z
day: '01'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1016/j.cnsns.2024.108011
ec_funded: 1
external_id:
  arxiv:
  - '2311.04114'
  isi:
  - '001238294600001'
file:
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  file_id: '18795'
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intvolume: '       134'
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month: '07'
oa: 1
oa_version: Published Version
project:
- _id: fc2ed2f7-9c52-11eb-aca3-c01059dda49c
  call_identifier: H2020
  grant_number: '101034413'
  name: 'IST-BRIDGE: International postdoctoral program'
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Communications in Nonlinear Science and Numerical Simulation
publication_identifier:
  issn:
  - 1007-5704
publication_status: published
publisher: Elsevier
quality_controlled: '1'
scopus_import: '1'
status: public
title: Dynamics and scaling of internally cooled convection
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 134
year: '2024'
...
---
_id: '17396'
abstract:
- lang: eng
  text: Wildfire intensity and severity have been increasing in the Iberian Peninsula
    in recent years, particularly in the Galicia region, due to rising temperatures
    and accumulating drier combustible vegetation in unmanaged lands. This leads to
    substantial emissions of air pollutants, notably fine particles (PM2.5), posing
    a risk to public health. This study aims to assess the impact of local and regional
    wildfires on PM2.5 levels in Galicia's main cities and their implications for
    air quality and public health. Over a decade (2013–2022), PM2.5 data during wildfire
    seasons were analyzed using statistical methods and Lagrangian tracking to monitor
    smoke plume evolution. The results reveal a notable increase in PM2.5 concentration
    during the wildfire season (June–November) in Galicia, surpassing health guidelines
    during extreme events and posing a significant health risk to the population.
    Regional wildfire analyses indicate that smoke plumes from Northern Portugal contribute
    to pollution in Galician cities, influencing the seasonality of heightened PM2.5
    levels. During extensive wildfires, elevated PM2.5 concentration values persisted
    for several days, potentially exacerbating health concerns in Galicia. These findings
    underscore the urgency of implementing air pollution prevention and management
    measures in the region, including developing effective alerts for large-scale
    events and improved wildfire management strategies to mitigate their impact on
    air quality in Galician cities.
acknowledgement: 'Alejandro Casallas was partially funded by a fellowship from the
  Abdus Salam International Centre for Theoretical Physics – ICTP. This project has
  received funding from the European Union’s Horizon 2020 research and innovation
  programme under the Marie Skłodowska-Curie grant agreement No 101034413 awarded
  to Alejandro Casallas. '
article_number: '122093'
article_processing_charge: Yes (in subscription journal)
article_type: original
author:
- first_name: César
  full_name: Quishpe-Vásquez, César
  last_name: Quishpe-Vásquez
- first_name: Patricia
  full_name: Oliva, Patricia
  last_name: Oliva
- first_name: Ellie Anne
  full_name: López-Barrera, Ellie Anne
  last_name: López-Barrera
- first_name: Alejandro
  full_name: Casallas Garcia, Alejandro
  id: 92081129-2d75-11ef-a48d-b04dd7a2385a
  last_name: Casallas Garcia
  orcid: 0000-0002-1988-5035
citation:
  ama: Quishpe-Vásquez C, Oliva P, López-Barrera EA, Casallas Garcia A. Wildfires
    impact on PM2.5 concentration in galicia Spain. <i>Journal of Environmental Management</i>.
    2024;367. doi:<a href="https://doi.org/10.1016/j.jenvman.2024.122093">10.1016/j.jenvman.2024.122093</a>
  apa: Quishpe-Vásquez, C., Oliva, P., López-Barrera, E. A., &#38; Casallas Garcia,
    A. (2024). Wildfires impact on PM2.5 concentration in galicia Spain. <i>Journal
    of Environmental Management</i>. Elsevier. <a href="https://doi.org/10.1016/j.jenvman.2024.122093">https://doi.org/10.1016/j.jenvman.2024.122093</a>
  chicago: Quishpe-Vásquez, César, Patricia Oliva, Ellie Anne López-Barrera, and Alejandro
    Casallas Garcia. “Wildfires Impact on PM2.5 Concentration in Galicia Spain.” <i>Journal
    of Environmental Management</i>. Elsevier, 2024. <a href="https://doi.org/10.1016/j.jenvman.2024.122093">https://doi.org/10.1016/j.jenvman.2024.122093</a>.
  ieee: C. Quishpe-Vásquez, P. Oliva, E. A. López-Barrera, and A. Casallas Garcia,
    “Wildfires impact on PM2.5 concentration in galicia Spain,” <i>Journal of Environmental
    Management</i>, vol. 367. Elsevier, 2024.
  ista: Quishpe-Vásquez C, Oliva P, López-Barrera EA, Casallas Garcia A. 2024. Wildfires
    impact on PM2.5 concentration in galicia Spain. Journal of Environmental Management.
    367, 122093.
  mla: Quishpe-Vásquez, César, et al. “Wildfires Impact on PM2.5 Concentration in
    Galicia Spain.” <i>Journal of Environmental Management</i>, vol. 367, 122093,
    Elsevier, 2024, doi:<a href="https://doi.org/10.1016/j.jenvman.2024.122093">10.1016/j.jenvman.2024.122093</a>.
  short: C. Quishpe-Vásquez, P. Oliva, E.A. López-Barrera, A. Casallas Garcia, Journal
    of Environmental Management 367 (2024).
date_created: 2024-08-06T05:54:52Z
date_published: 2024-09-01T00:00:00Z
date_updated: 2025-09-08T08:53:10Z
day: '01'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1016/j.jenvman.2024.122093
ec_funded: 1
external_id:
  isi:
  - '001289532100001'
  pmid:
  - '39106804'
file:
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  checksum: 6fa476a4c08aded413844d92336b0e52
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  creator: acasalla
  date_created: 2024-08-09T13:37:23Z
  date_updated: 2024-08-09T13:37:23Z
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file_date_updated: 2024-08-09T13:37:24Z
has_accepted_license: '1'
intvolume: '       367'
isi: 1
language:
- iso: eng
license: https://creativecommons.org/licenses/by-nc/4.0/
month: '09'
oa: 1
oa_version: Published Version
pmid: 1
project:
- _id: fc2ed2f7-9c52-11eb-aca3-c01059dda49c
  call_identifier: H2020
  grant_number: '101034413'
  name: 'IST-BRIDGE: International postdoctoral program'
publication: Journal of Environmental Management
publication_identifier:
  issn:
  - 0301-4797
publication_status: published
publisher: Elsevier
quality_controlled: '1'
scopus_import: '1'
status: public
title: Wildfires impact on PM2.5 concentration in galicia Spain
tmp:
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type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 367
year: '2024'
...
---
_id: '17435'
abstract:
- lang: eng
  text: 'The Mediterranean region is experiencing pronounced aridification and in
    certain areas higher occurrence of intense precipitation. In this work, we analyze
    the evolution of the precipitation probability distribution in terms of precipitating
    days (or “wet-days”) and all-days quantile trends, in Europe and the Mediterranean,
    using the ERA5 reanalysis. Looking at the form of wet-days quantile trends curves,
    we identify four regimes. Two are predominant: in most of northern Europe the
    precipitation quantiles all intensify, while in the Mediterranean the low-medium
    quantiles are mostly decreasing as extremes intensify or decrease. The wet-days
    distribution is then modeled by a Weibull law with two parameters, whose changes
    capture the four regimes. Assessing the significance of the parameters'' changes
    over 1950–2020 shows that a signal on wet-days distribution has already emerged
    in northern Europe (where the distribution shifts to more intense precipitation),
    but not yet in the Mediterranean, where the natural variability is stronger. We
    extend the results by describing the all-days distribution change as the wet-days’
    change plus a contribution from the dry-days frequency change, and study their
    relative contribution. In northern Europe, the wet-days distribution change is
    the dominant driver, and the contribution of dry-days frequency change can be
    neglected for wet-days percentiles above about 50%. In the Mediterranean, however,
    the change of precipitation distribution comes from the significant increase of
    dry-days frequency instead of an intensity change during wet-days. Therefore,
    in the Mediterranean the increase of dry-days frequency is crucial for all-days
    trends, even for heavy precipitation.'
acknowledgement: CJM gratefully acknowledge funding from the European Research Council
  (ERC) under the European Union's Horizon 2020 research and innovation program (Project
  CLUSTER, Grant Agreement No 805041). The authors also thank Samuel Somot (Centre
  National de Recherches Météorologiques, Toulouse) and Juliette Blanchet (Institut
  des Géosciences de l’Environnement, Grenoble) for their fruitful discussions on
  the project.
article_number: e2023JD040413
article_processing_charge: Yes (in subscription journal)
article_type: original
author:
- first_name: Julie
  full_name: André, Julie
  last_name: André
- first_name: Fabio
  full_name: D'Andrea, Fabio
  last_name: D'Andrea
- first_name: Philippe
  full_name: Drobinski, Philippe
  last_name: Drobinski
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
citation:
  ama: 'André J, D’Andrea F, Drobinski P, Muller CJ. Regimes of precipitation change
    over Europe and the Mediterranean. <i>Journal of Geophysical Research: Atmospheres</i>.
    2024;129(15). doi:<a href="https://doi.org/10.1029/2023JD040413">10.1029/2023JD040413</a>'
  apa: 'André, J., D’Andrea, F., Drobinski, P., &#38; Muller, C. J. (2024). Regimes
    of precipitation change over Europe and the Mediterranean. <i>Journal of Geophysical
    Research: Atmospheres</i>. Wiley. <a href="https://doi.org/10.1029/2023JD040413">https://doi.org/10.1029/2023JD040413</a>'
  chicago: 'André, Julie, Fabio D’Andrea, Philippe Drobinski, and Caroline J Muller.
    “Regimes of Precipitation Change over Europe and the Mediterranean.” <i>Journal
    of Geophysical Research: Atmospheres</i>. Wiley, 2024. <a href="https://doi.org/10.1029/2023JD040413">https://doi.org/10.1029/2023JD040413</a>.'
  ieee: 'J. André, F. D’Andrea, P. Drobinski, and C. J. Muller, “Regimes of precipitation
    change over Europe and the Mediterranean,” <i>Journal of Geophysical Research:
    Atmospheres</i>, vol. 129, no. 15. Wiley, 2024.'
  ista: 'André J, D’Andrea F, Drobinski P, Muller CJ. 2024. Regimes of precipitation
    change over Europe and the Mediterranean. Journal of Geophysical Research: Atmospheres.
    129(15), e2023JD040413.'
  mla: 'André, Julie, et al. “Regimes of Precipitation Change over Europe and the
    Mediterranean.” <i>Journal of Geophysical Research: Atmospheres</i>, vol. 129,
    no. 15, e2023JD040413, Wiley, 2024, doi:<a href="https://doi.org/10.1029/2023JD040413">10.1029/2023JD040413</a>.'
  short: 'J. André, F. D’Andrea, P. Drobinski, C.J. Muller, Journal of Geophysical
    Research: Atmospheres 129 (2024).'
date_created: 2024-08-18T22:01:04Z
date_published: 2024-08-16T00:00:00Z
date_updated: 2025-09-08T08:56:53Z
day: '16'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2023JD040413
ec_funded: 1
external_id:
  isi:
  - '001285897600001'
file:
- access_level: open_access
  checksum: 71d7f966318e11ce474737f4e37405ef
  content_type: application/pdf
  creator: dernst
  date_created: 2024-08-19T06:32:21Z
  date_updated: 2024-08-19T06:32:21Z
  file_id: '17438'
  file_name: 2024_JGRAtmospheres_Andre.pdf
  file_size: 8126046
  relation: main_file
  success: 1
file_date_updated: 2024-08-19T06:32:21Z
has_accepted_license: '1'
intvolume: '       129'
isi: 1
issue: '15'
language:
- iso: eng
month: '08'
oa: 1
oa_version: Published Version
project:
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: 'Journal of Geophysical Research: Atmospheres'
publication_identifier:
  eissn:
  - 2169-8996
  issn:
  - 2169-897X
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: Regimes of precipitation change over Europe and the Mediterranean
tmp:
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  short: CC BY-NC (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 129
year: '2024'
...
---
_id: '14453'
abstract:
- lang: eng
  text: Squall lines are substantially influenced by the interaction of low-level
    shear with cold pools associated with convective downdrafts. Beyond an optimal
    shear amplitude, squall lines tend to orient themselves at an angle with respect
    to the low-level shear. While the mechanisms behind squall line orientation seem
    to be increasingly well understood, uncertainties remain on the implications of
    this orientation. Roca and Fiolleau (2020, https://doi.org/10.1038/s43247-020-00015-4)
    show that long lived mesoscale convective systems, including squall lines, are
    disproportionately involved in rainfall extremes in the tropics. This article
    investigates the influence of the interaction between low-level shear and squall
    line outflow on squall line generated precipitation extrema in the tropics. Using
    a cloud resolving model, simulated squall lines in radiative convective equilibrium
    amid a shear-dominated regime (super optimal), a balanced regime (optimal), and
    an outflow dominated regime (suboptimal). Our results show that precipitation
    extremes in squall lines are 40% more intense in the case of optimal shear and
    remain 30% superior in the superoptimal regime relative to a disorganized case.
    With a theoretical scaling of precipitation extremes (C. Muller & Takayabu, 2020,
    https://doi.org/10.1088/1748-9326/ab7130), we show that the condensation rates
    control the amplification of precipitation extremes in tropical squall lines,
    mainly due to its change in vertical mass flux (dynamic component). The reduction
    of dilution by entrainment explains half of this change, consistent with Mulholland
    et al. (2021, https://doi.org/10.1175/jas-d-20-0299.1). The other half is explained
    by increased cloud-base velocity intensity in optimal and superoptimal squall
    lines.
acknowledgement: The authors gratefully acknowledge funding from the European Research
  Council under the European Union's Horizon 2020 research and innovation program
  (Project CLUSTER, Grant Agreement No. 805041). This work is also supported by a
  PhD fellowship funded by the Ecole Normale Supérieure de Paris-Saclay. Authors are
  also grateful to Benjamin Filider, who was of great help and support in the development
  of ideas. Eventually, we would like to thank Martin Singh, John M. Peters and an
  anonymous reviewer for their valuable comments and suggestions, which greatly improved
  the quality of the manuscript.
article_number: e2022MS003477
article_processing_charge: Yes
article_type: original
author:
- first_name: Sophie
  full_name: Abramian, Sophie
  last_name: Abramian
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
- first_name: Camille
  full_name: Risi, Camille
  last_name: Risi
citation:
  ama: Abramian S, Muller CJ, Risi C. Extreme precipitation in tropical squall lines.
    <i>Journal of Advances in Modeling Earth Systems</i>. 2023;15(10). doi:<a href="https://doi.org/10.1029/2022MS003477">10.1029/2022MS003477</a>
  apa: Abramian, S., Muller, C. J., &#38; Risi, C. (2023). Extreme precipitation in
    tropical squall lines. <i>Journal of Advances in Modeling Earth Systems</i>. Wiley.
    <a href="https://doi.org/10.1029/2022MS003477">https://doi.org/10.1029/2022MS003477</a>
  chicago: Abramian, Sophie, Caroline J Muller, and Camille Risi. “Extreme Precipitation
    in Tropical Squall Lines.” <i>Journal of Advances in Modeling Earth Systems</i>.
    Wiley, 2023. <a href="https://doi.org/10.1029/2022MS003477">https://doi.org/10.1029/2022MS003477</a>.
  ieee: S. Abramian, C. J. Muller, and C. Risi, “Extreme precipitation in tropical
    squall lines,” <i>Journal of Advances in Modeling Earth Systems</i>, vol. 15,
    no. 10. Wiley, 2023.
  ista: Abramian S, Muller CJ, Risi C. 2023. Extreme precipitation in tropical squall
    lines. Journal of Advances in Modeling Earth Systems. 15(10), e2022MS003477.
  mla: Abramian, Sophie, et al. “Extreme Precipitation in Tropical Squall Lines.”
    <i>Journal of Advances in Modeling Earth Systems</i>, vol. 15, no. 10, e2022MS003477,
    Wiley, 2023, doi:<a href="https://doi.org/10.1029/2022MS003477">10.1029/2022MS003477</a>.
  short: S. Abramian, C.J. Muller, C. Risi, Journal of Advances in Modeling Earth
    Systems 15 (2023).
date_created: 2023-10-29T23:01:15Z
date_published: 2023-10-01T00:00:00Z
date_updated: 2024-11-05T09:00:44Z
day: '01'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2022MS003477
ec_funded: 1
external_id:
  isi:
  - '001084933600001'
file:
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file_date_updated: 2023-10-30T13:31:42Z
has_accepted_license: '1'
intvolume: '        15'
isi: 1
issue: '10'
language:
- iso: eng
month: '10'
oa: 1
oa_version: Published Version
project:
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Journal of Advances in Modeling Earth Systems
publication_identifier:
  eissn:
  - 1942-2466
publication_status: published
publisher: Wiley
quality_controlled: '1'
scopus_import: '1'
status: public
title: Extreme precipitation in tropical squall lines
tmp:
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  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 15
year: '2023'
...
---
_id: '14564'
abstract:
- lang: eng
  text: Cumulus parameterization (CP) in state‐of‐the‐art global climate models is
    based on the quasi‐equilibrium assumption (QEA), which views convection as the
    action of an ensemble of cumulus clouds, in a state of equilibrium with respect
    to a slowly varying atmospheric state. This view is not compatible with the organization
    and dynamical interactions across multiple scales of cloud systems in the tropics
    and progress in this research area was slow over decades despite the widely recognized
    major shortcomings. Novel ideas on how to represent key physical processes of
    moist convection‐large‐scale interaction to overcome the QEA have surged recently.
    The stochastic multicloud model (SMCM) CP in particular mimics the dynamical interactions
    of multiple cloud types that characterize organized tropical convection. Here,
    the SMCM is used to modify the Zhang‐McFarlane (ZM) CP by changing the way in
    which the bulk mass flux and bulk entrainment and detrainment rates are calculated.
    This is done by introducing a stochastic ensemble of plumes characterized by randomly
    varying detrainment level distributions based on the cloud area fraction of the
    SMCM. The SMCM is here extended to include shallow cumulus clouds resulting in
    a unified shallow‐deep CP. The new stochastic multicloud plume CP is validated
    against the control ZM scheme in the context of the single column Community Climate
    Model of the National Center for Atmospheric Research using data from both tropical
    ocean and midlatitude land convection. Some key features of the SMCM CP such as
    it capability to represent the tri‐modal nature of organized convection are emphasized.
acknowledgement: The research of B.K. is supported in part by a Discovery Grant from
  the Natural Sciences and Engineering Research Council of Canada (RGPIN-04246-2020).
  This research was conducted during the visits of P.M. Krishna to the Center for
  Prototype Climate Models at NYU Abu Dhabi and University of Victoria from November
  2018 to June 2019 and July 2019 and October 2019, respectively. The authors are
  very grateful to the three anonymous reviewers who provided very thoughtful and
  constructive comments during the review process that helped greatly improve and
  shape the final version of the manuscript.
article_number: e2022MS003391
article_processing_charge: Yes
article_type: original
author:
- first_name: B.
  full_name: Khouider, B.
  last_name: Khouider
- first_name: BIDYUT B
  full_name: GOSWAMI, BIDYUT B
  id: 3a4ac09c-6d61-11ec-bf66-884cde66b64b
  last_name: GOSWAMI
  orcid: 0000-0001-8602-3083
- first_name: R.
  full_name: Phani, R.
  last_name: Phani
- first_name: A. J.
  full_name: Majda, A. J.
  last_name: Majda
citation:
  ama: Khouider B, GOSWAMI BB, Phani R, Majda AJ. A shallow‐deep unified stochastic
    mass flux cumulus parameterization in the single column community climate model.
    <i>Journal of Advances in Modeling Earth Systems</i>. 2023;15(11). doi:<a href="https://doi.org/10.1029/2022ms003391">10.1029/2022ms003391</a>
  apa: Khouider, B., GOSWAMI, B. B., Phani, R., &#38; Majda, A. J. (2023). A shallow‐deep
    unified stochastic mass flux cumulus parameterization in the single column community
    climate model. <i>Journal of Advances in Modeling Earth Systems</i>. American
    Geophysical Union. <a href="https://doi.org/10.1029/2022ms003391">https://doi.org/10.1029/2022ms003391</a>
  chicago: Khouider, B., BIDYUT B GOSWAMI, R. Phani, and A. J. Majda. “A Shallow‐deep
    Unified Stochastic Mass Flux Cumulus Parameterization in the Single Column Community
    Climate Model.” <i>Journal of Advances in Modeling Earth Systems</i>. American
    Geophysical Union, 2023. <a href="https://doi.org/10.1029/2022ms003391">https://doi.org/10.1029/2022ms003391</a>.
  ieee: B. Khouider, B. B. GOSWAMI, R. Phani, and A. J. Majda, “A shallow‐deep unified
    stochastic mass flux cumulus parameterization in the single column community climate
    model,” <i>Journal of Advances in Modeling Earth Systems</i>, vol. 15, no. 11.
    American Geophysical Union, 2023.
  ista: Khouider B, GOSWAMI BB, Phani R, Majda AJ. 2023. A shallow‐deep unified stochastic
    mass flux cumulus parameterization in the single column community climate model.
    Journal of Advances in Modeling Earth Systems. 15(11), e2022MS003391.
  mla: Khouider, B., et al. “A Shallow‐deep Unified Stochastic Mass Flux Cumulus Parameterization
    in the Single Column Community Climate Model.” <i>Journal of Advances in Modeling
    Earth Systems</i>, vol. 15, no. 11, e2022MS003391, American Geophysical Union,
    2023, doi:<a href="https://doi.org/10.1029/2022ms003391">10.1029/2022ms003391</a>.
  short: B. Khouider, B.B. GOSWAMI, R. Phani, A.J. Majda, Journal of Advances in Modeling
    Earth Systems 15 (2023).
date_created: 2023-11-20T09:18:21Z
date_published: 2023-11-01T00:00:00Z
date_updated: 2025-09-09T13:29:45Z
day: '01'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2022ms003391
external_id:
  isi:
  - '001106311000001'
file:
- access_level: open_access
  checksum: e30329dd985559de0ddc7021ca7382b4
  content_type: application/pdf
  creator: dernst
  date_created: 2023-11-20T11:29:16Z
  date_updated: 2023-11-20T11:29:16Z
  file_id: '14582'
  file_name: 2023_JAMES_Khoulder.pdf
  file_size: 6435697
  relation: main_file
  success: 1
file_date_updated: 2023-11-20T11:29:16Z
has_accepted_license: '1'
intvolume: '        15'
isi: 1
issue: '11'
keyword:
- General Earth and Planetary Sciences
- Environmental Chemistry
- Global and Planetary Change
language:
- iso: eng
month: '11'
oa: 1
oa_version: Published Version
publication: Journal of Advances in Modeling Earth Systems
publication_identifier:
  eissn:
  - 1942-2466
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
scopus_import: '1'
status: public
title: A shallow‐deep unified stochastic mass flux cumulus parameterization in the
  single column community climate model
tmp:
  image: /images/cc_by_nc.png
  legal_code_url: https://creativecommons.org/licenses/by-nc/4.0/legalcode
  name: Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
  short: CC BY-NC (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 15
year: '2023'
...
---
_id: '14654'
abstract:
- lang: eng
  text: Two assumptions commonly applied in convection schemes—the diagnostic and
    quasi-equilibrium assumptions—imply that convective activity (e.g., convective
    precipitation) is controlled only by the large-scale (macrostate) environment
    at the time. In contrast, numerical experiments indicate a “memory” or dependence
    of convection also on its own previous activity whereby subgrid-scale (microstate)
    structures boost but are also boosted by convection. In this study we investigated
    this memory by comparing single-column model behavior in two idealized tests previously
    executed by a cloud-resolving model (CRM). Conventional convection schemes that
    employ the diagnostic assumption fail to reproduce the CRM behavior. The memory-capable
    org and Laboratoire de Météorologie Dynamique Zoom cold pool schemes partially
    capture the behavior, but fail to fully exhibit the strong reinforcing feedbacks
    implied by the CRM. Analysis of this failure suggests that it is because the CRM
    supports a linear (or superlinear) dependence of the subgrid structure growth
    rate on the precipitation rate, while the org scheme assumes a sublinear dependence.
    Among varying versions of the org scheme, the growth rate of the org variable
    representing subgrid structure is strongly associated with memory strength. These
    results demonstrate the importance of parameterizing convective memory, and the
    ability of idealized tests to reveal shortcomings of convection schemes and constrain
    model structural assumptions.
acknowledgement: YLH is supported by funding from the European Union's Horizon 2020
  research and innovation programme under the Marie Skłodowska-Curie Grant Agreement
  No. 101034413. CJM gratefully acknowledges funding from the European Research Council
  under the European Union's Horizon 2020 research and innovation program (Project
  CLUSTER, Grant Agreement No. 805041). YLH and SCS were supported by the Australian
  Research Council (FL150100035). The authors thank Brian Mapes, David Fuchs and Siwon
  Song for stimulating and helpful discussions. MC warmly thanks the LMD team in Paris
  for their assistance with the LMDZ model. We thank the two anonymous reviewers for
  their constructive comments that greatly improved this manuscript.
article_number: e2023MS003726
article_processing_charge: Yes
article_type: original
author:
- first_name: Yi-Ling
  full_name: Hwong, Yi-Ling
  id: 1217aa61-4dd1-11ec-9ac3-f2ba3f17ee22
  last_name: Hwong
  orcid: 0000-0001-9281-3479
- first_name: M.
  full_name: Colin, M.
  last_name: Colin
- first_name: Philipp
  full_name: Aglas, Philipp
  id: 02eace56-97fc-11ee-b81a-f0939ca85a77
  last_name: Aglas
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
- first_name: S. C.
  full_name: Sherwood, S. C.
  last_name: Sherwood
citation:
  ama: Hwong Y-L, Colin M, Aglas P, Muller CJ, Sherwood SC. Assessing memory in convection
    schemes using idealized tests. <i>Journal of Advances in Modeling Earth Systems</i>.
    2023;15(12). doi:<a href="https://doi.org/10.1029/2023MS003726">10.1029/2023MS003726</a>
  apa: Hwong, Y.-L., Colin, M., Aglas, P., Muller, C. J., &#38; Sherwood, S. C. (2023).
    Assessing memory in convection schemes using idealized tests. <i>Journal of Advances
    in Modeling Earth Systems</i>. Wiley. <a href="https://doi.org/10.1029/2023MS003726">https://doi.org/10.1029/2023MS003726</a>
  chicago: Hwong, Yi-Ling, M. Colin, Philipp Aglas, Caroline J Muller, and S. C. Sherwood.
    “Assessing Memory in Convection Schemes Using Idealized Tests.” <i>Journal of
    Advances in Modeling Earth Systems</i>. Wiley, 2023. <a href="https://doi.org/10.1029/2023MS003726">https://doi.org/10.1029/2023MS003726</a>.
  ieee: Y.-L. Hwong, M. Colin, P. Aglas, C. J. Muller, and S. C. Sherwood, “Assessing
    memory in convection schemes using idealized tests,” <i>Journal of Advances in
    Modeling Earth Systems</i>, vol. 15, no. 12. Wiley, 2023.
  ista: Hwong Y-L, Colin M, Aglas P, Muller CJ, Sherwood SC. 2023. Assessing memory
    in convection schemes using idealized tests. Journal of Advances in Modeling Earth
    Systems. 15(12), e2023MS003726.
  mla: Hwong, Yi-Ling, et al. “Assessing Memory in Convection Schemes Using Idealized
    Tests.” <i>Journal of Advances in Modeling Earth Systems</i>, vol. 15, no. 12,
    e2023MS003726, Wiley, 2023, doi:<a href="https://doi.org/10.1029/2023MS003726">10.1029/2023MS003726</a>.
  short: Y.-L. Hwong, M. Colin, P. Aglas, C.J. Muller, S.C. Sherwood, Journal of Advances
    in Modeling Earth Systems 15 (2023).
corr_author: '1'
date_created: 2023-12-10T23:00:57Z
date_published: 2023-12-01T00:00:00Z
date_updated: 2025-09-09T13:35:40Z
day: '01'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2023MS003726
ec_funded: 1
external_id:
  isi:
  - '001110801100001'
file:
- access_level: open_access
  checksum: 4d060b293da3d203de8769e398edf711
  content_type: application/pdf
  creator: dernst
  date_created: 2023-12-11T08:08:44Z
  date_updated: 2023-12-11T08:08:44Z
  file_id: '14670'
  file_name: 2023_JAMES_Hwong.pdf
  file_size: 2783677
  relation: main_file
  success: 1
file_date_updated: 2023-12-11T08:08:44Z
has_accepted_license: '1'
intvolume: '        15'
isi: 1
issue: '12'
language:
- iso: eng
month: '12'
oa: 1
oa_version: Published Version
project:
- _id: 629205d8-2b32-11ec-9570-e1356ff73576
  call_identifier: H2020
  grant_number: '805041'
  name: Organization of CLoUdS, and implications of Tropical  cyclones and for the
    Energetics of the tropics, in current and waRming climate
publication: Journal of Advances in Modeling Earth Systems
publication_identifier:
  eissn:
  - 1942-2466
publication_status: published
publisher: Wiley
quality_controlled: '1'
related_material:
  record:
  - id: '14991'
    relation: research_data
    status: public
scopus_import: '1'
status: public
title: Assessing memory in convection schemes using idealized tests
tmp:
  image: /images/cc_by_nc_nd.png
  legal_code_url: https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
  name: Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
    (CC BY-NC-ND 4.0)
  short: CC BY-NC-ND (4.0)
type: journal_article
user_id: 317138e5-6ab7-11ef-aa6d-ffef3953e345
volume: 15
year: '2023'
...
---
_id: '12791'
abstract:
- lang: eng
  text: We investigate the capabilities of Physics-Informed Neural Networks (PINNs)
    to reconstruct turbulent Rayleigh–Bénard flows using only temperature information.
    We perform a quantitative analysis of the quality of the reconstructions at various
    amounts of low-passed-filtered information and turbulent intensities. We compare
    our results with those obtained via nudging, a classical equation-informed data
    assimilation technique. At low Rayleigh numbers, PINNs are able to reconstruct
    with high precision, comparable to the one achieved with nudging. At high Rayleigh
    numbers, PINNs outperform nudging and are able to achieve satisfactory reconstruction
    of the velocity fields only when data for temperature is provided with high spatial
    and temporal density. When data becomes sparse, the PINNs performance worsens,
    not only in a point-to-point error sense but also, and contrary to nudging, in
    a statistical sense, as can be seen in the probability density functions and energy
    spectra.
acknowledgement: This project has received partial funding from the European Research
  Council (ERC) under the European Union’s Horizon 2020 Research and Innovation Programme
  (Grant Agreement No. 882340))
article_number: '16'
article_processing_charge: No
article_type: original
arxiv: 1
author:
- first_name: Patricio
  full_name: Clark Di Leoni, Patricio
  last_name: Clark Di Leoni
- first_name: Lokahith N
  full_name: Agasthya, Lokahith N
  id: cd100965-0804-11ed-9c55-f4878ff4e877
  last_name: Agasthya
- first_name: Michele
  full_name: Buzzicotti, Michele
  last_name: Buzzicotti
- first_name: Luca
  full_name: Biferale, Luca
  last_name: Biferale
citation:
  ama: Clark Di Leoni P, Agasthya LN, Buzzicotti M, Biferale L. Reconstructing Rayleigh–Bénard
    flows out of temperature-only measurements using Physics-Informed Neural Networks.
    <i>The European Physical Journal E</i>. 2023;46(3). doi:<a href="https://doi.org/10.1140/epje/s10189-023-00276-9">10.1140/epje/s10189-023-00276-9</a>
  apa: Clark Di Leoni, P., Agasthya, L. N., Buzzicotti, M., &#38; Biferale, L. (2023).
    Reconstructing Rayleigh–Bénard flows out of temperature-only measurements using
    Physics-Informed Neural Networks. <i>The European Physical Journal E</i>. Springer
    Nature. <a href="https://doi.org/10.1140/epje/s10189-023-00276-9">https://doi.org/10.1140/epje/s10189-023-00276-9</a>
  chicago: Clark Di Leoni, Patricio, Lokahith N Agasthya, Michele Buzzicotti, and
    Luca Biferale. “Reconstructing Rayleigh–Bénard Flows out of Temperature-Only Measurements
    Using Physics-Informed Neural Networks.” <i>The European Physical Journal E</i>.
    Springer Nature, 2023. <a href="https://doi.org/10.1140/epje/s10189-023-00276-9">https://doi.org/10.1140/epje/s10189-023-00276-9</a>.
  ieee: P. Clark Di Leoni, L. N. Agasthya, M. Buzzicotti, and L. Biferale, “Reconstructing
    Rayleigh–Bénard flows out of temperature-only measurements using Physics-Informed
    Neural Networks,” <i>The European Physical Journal E</i>, vol. 46, no. 3. Springer
    Nature, 2023.
  ista: Clark Di Leoni P, Agasthya LN, Buzzicotti M, Biferale L. 2023. Reconstructing
    Rayleigh–Bénard flows out of temperature-only measurements using Physics-Informed
    Neural Networks. The European Physical Journal E. 46(3), 16.
  mla: Clark Di Leoni, Patricio, et al. “Reconstructing Rayleigh–Bénard Flows out
    of Temperature-Only Measurements Using Physics-Informed Neural Networks.” <i>The
    European Physical Journal E</i>, vol. 46, no. 3, 16, Springer Nature, 2023, doi:<a
    href="https://doi.org/10.1140/epje/s10189-023-00276-9">10.1140/epje/s10189-023-00276-9</a>.
  short: P. Clark Di Leoni, L.N. Agasthya, M. Buzzicotti, L. Biferale, The European
    Physical Journal E 46 (2023).
date_created: 2023-04-02T22:01:11Z
date_published: 2023-03-20T00:00:00Z
date_updated: 2025-04-23T08:52:35Z
day: '20'
department:
- _id: CaMu
doi: 10.1140/epje/s10189-023-00276-9
external_id:
  arxiv:
  - '2301.07769'
  isi:
  - '000956387200001'
  pmid:
  - '36939938'
intvolume: '        46'
isi: 1
issue: '3'
language:
- iso: eng
main_file_link:
- open_access: '1'
  url: ' https://doi.org/10.48550/arXiv.2301.07769'
month: '03'
oa: 1
oa_version: Preprint
pmid: 1
publication: The European Physical Journal E
publication_identifier:
  eissn:
  - 1292-895X
  issn:
  - 1292-8941
publication_status: published
publisher: Springer Nature
quality_controlled: '1'
scopus_import: '1'
status: public
title: Reconstructing Rayleigh–Bénard flows out of temperature-only measurements using
  Physics-Informed Neural Networks
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 46
year: '2023'
...
---
_id: '13256'
abstract:
- lang: eng
  text: The El Niño-Southern Oscillation (ENSO) and the Indian summer monsoon (ISM,
    or monsoon) are two giants of tropical climate. Here we assess the future evolution
    of the ENSO-monsoon teleconnection in climate simulations with idealized forcing
    of CO2 increment at a rate of 1% year-1 starting from a present-day condition
    (367 p.p.m.) until quadrupling. We find a monotonous weakening of the ENSO-monsoon
    teleconnection with the increase in CO2. Increased co-occurrences of El Niño and
    positive Indian Ocean Dipoles (pIODs) in a warmer climate weaken the teleconnection.
    Co-occurrences of El Niño and pIOD are attributable to mean sea surface temperature
    (SST) warming that resembles a pIOD-type warming pattern in the Indian Ocean and
    an El Niño-type warming in the Pacific. Since ENSO is a critical precursor of
    the strength of the Indian monsoon, a weakening of this relation may mean a less
    predictable Indian monsoon in a warmer climate.
acknowledgement: This work was supported by National Research Foundation of Korea
  (NRF) grants funded by the Korean government (MSIT) (NRF-2018R1A5A1024958, RS-2023-00208000).
  Model simulation and data transfer were supported by the National Supercomputing
  Center with supercomputing resources including technical support (KSC-2019-CHA-0005),
  the National Center for Meteorological Supercomputer of the Korea Meteorological
  Administration (KMA), and by the Korea Research Environment Open NETwork (KREONET),
  respectively. We sincerely thank Dr. Jongsoo Shin of Pohang University of Science
  and Technology, Pohang, South Korea for the model simulations.
article_number: '82'
article_processing_charge: Yes
article_type: original
author:
- first_name: Bidyut B
  full_name: Goswami, Bidyut B
  id: 3a4ac09c-6d61-11ec-bf66-884cde66b64b
  last_name: Goswami
- first_name: Soon Il
  full_name: An, Soon Il
  last_name: An
citation:
  ama: GOSWAMI BB, An SI. An assessment of the ENSO-monsoon teleconnection in a warming
    climate. <i>npj Climate and Atmospheric Science</i>. 2023;6. doi:<a href="https://doi.org/10.1038/s41612-023-00411-5">10.1038/s41612-023-00411-5</a>
  apa: GOSWAMI, B. B., &#38; An, S. I. (2023). An assessment of the ENSO-monsoon teleconnection
    in a warming climate. <i>Npj Climate and Atmospheric Science</i>. Springer Nature.
    <a href="https://doi.org/10.1038/s41612-023-00411-5">https://doi.org/10.1038/s41612-023-00411-5</a>
  chicago: GOSWAMI, BIDYUT B, and Soon Il An. “An Assessment of the ENSO-Monsoon Teleconnection
    in a Warming Climate.” <i>Npj Climate and Atmospheric Science</i>. Springer Nature,
    2023. <a href="https://doi.org/10.1038/s41612-023-00411-5">https://doi.org/10.1038/s41612-023-00411-5</a>.
  ieee: B. B. GOSWAMI and S. I. An, “An assessment of the ENSO-monsoon teleconnection
    in a warming climate,” <i>npj Climate and Atmospheric Science</i>, vol. 6. Springer
    Nature, 2023.
  ista: GOSWAMI BB, An SI. 2023. An assessment of the ENSO-monsoon teleconnection
    in a warming climate. npj Climate and Atmospheric Science. 6, 82.
  mla: GOSWAMI, BIDYUT B., and Soon Il An. “An Assessment of the ENSO-Monsoon Teleconnection
    in a Warming Climate.” <i>Npj Climate and Atmospheric Science</i>, vol. 6, 82,
    Springer Nature, 2023, doi:<a href="https://doi.org/10.1038/s41612-023-00411-5">10.1038/s41612-023-00411-5</a>.
  short: B.B. GOSWAMI, S.I. An, Npj Climate and Atmospheric Science 6 (2023).
date_created: 2023-07-23T22:01:10Z
date_published: 2023-07-08T00:00:00Z
date_updated: 2023-08-02T06:38:07Z
day: '08'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1038/s41612-023-00411-5
external_id:
  isi:
  - '001024920300002'
file:
- access_level: open_access
  checksum: e9967d436a83b8ffcc6f58782e1f7500
  content_type: application/pdf
  creator: dernst
  date_created: 2023-07-31T08:00:01Z
  date_updated: 2023-07-31T08:00:01Z
  file_id: '13326'
  file_name: 2023_npjclimate_Goswami.pdf
  file_size: 1750712
  relation: main_file
  success: 1
file_date_updated: 2023-07-31T08:00:01Z
has_accepted_license: '1'
intvolume: '         6'
isi: 1
language:
- iso: eng
month: '07'
oa: 1
oa_version: Published Version
publication: npj Climate and Atmospheric Science
publication_identifier:
  eissn:
  - 2397-3722
publication_status: published
publisher: Springer Nature
quality_controlled: '1'
scopus_import: '1'
status: public
title: An assessment of the ENSO-monsoon teleconnection in a warming climate
tmp:
  image: /images/cc_by.png
  legal_code_url: https://creativecommons.org/licenses/by/4.0/legalcode
  name: Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)
  short: CC BY (4.0)
type: journal_article
user_id: 4359f0d1-fa6c-11eb-b949-802e58b17ae8
volume: 6
year: '2023'
...
---
_id: '14752'
abstract:
- lang: eng
  text: 'Radiative cooling of the lowest atmospheric levels is of strong importance
    for modulating atmospheric circulations and organizing convection, but detailed
    observations and a robust theoretical understanding are lacking. Here we use unprecedented
    observational constraints from subsidence regimes in the tropical Atlantic to
    develop a theory for the shape and magnitude of low‐level longwave radiative cooling
    in clear‐sky, showing peaks larger than 5–10 K/day at the top of the boundary
    layer. A suite of novel scaling approximations is first developed from simplified
    spectral theory, in close agreement with the measurements. The radiative cooling
    peak height is set by the maximum lapse rate in water vapor path, and its magnitude
    is mainly controlled by the ratio of column relative humidity above and below
    the peak. We emphasize how elevated intrusions of moist air can reduce low‐level
    cooling, by sporadically shading the spectral range which effectively cools to
    space. The efficiency of this spectral shading depends both on water content and
    altitude of moist intrusions; its height dependence cannot be explained by the
    temperature difference between the emitting and absorbing layers, but by the decrease
    of water vapor extinction with altitude. This analytical work can help to narrow
    the search for low‐level cloud patterns sensitive to radiative‐convective feedbacks:
    the most organized patterns with largest cloud fractions occur in atmospheres
    below 10% relative humidity and feel the strongest low‐level cooling. This motivates
    further assessment of favorable conditions for radiative‐convective feedbacks
    and a robust quantification of corresponding shallow cloud dynamics in current
    and warmer climates.'
acknowledgement: The authors would like to thank two anonymous reviews and gratefully
  acknowledge diverse funding agencies and resources used for this work. B.F. and
  C.M. thank funding from the European Research Council (ERC) under the European Union's
  Horizon 2020 research and innovation program (Project CLUSTER, grant agreement no.
  805041), and the EUREC4A campaign organizers for giving the opportunity to take
  part to the campaign and use the data early on. R. P. was supported by the US National
  Science Foundation (award AGS 19–16908), by the National Oceanic and Atmospheric
  Administration (award NA200AR4310375), and the Vetlesen Foundation.
article_number: e2023AV000880
article_processing_charge: Yes
article_type: original
author:
- first_name: B.
  full_name: Fildier, B.
  last_name: Fildier
- first_name: Caroline J
  full_name: Muller, Caroline J
  id: f978ccb0-3f7f-11eb-b193-b0e2bd13182b
  last_name: Muller
  orcid: 0000-0001-5836-5350
- first_name: R.
  full_name: Pincus, R.
  last_name: Pincus
- first_name: S.
  full_name: Fueglistaler, S.
  last_name: Fueglistaler
citation:
  ama: Fildier B, Muller CJ, Pincus R, Fueglistaler S. How moisture shapes low‐level
    radiative cooling in subsidence regimes. <i>AGU Advances</i>. 2023;4(3). doi:<a
    href="https://doi.org/10.1029/2023av000880">10.1029/2023av000880</a>
  apa: Fildier, B., Muller, C. J., Pincus, R., &#38; Fueglistaler, S. (2023). How
    moisture shapes low‐level radiative cooling in subsidence regimes. <i>AGU Advances</i>.
    American Geophysical Union. <a href="https://doi.org/10.1029/2023av000880">https://doi.org/10.1029/2023av000880</a>
  chicago: Fildier, B., Caroline J Muller, R. Pincus, and S. Fueglistaler. “How Moisture
    Shapes Low‐level Radiative Cooling in Subsidence Regimes.” <i>AGU Advances</i>.
    American Geophysical Union, 2023. <a href="https://doi.org/10.1029/2023av000880">https://doi.org/10.1029/2023av000880</a>.
  ieee: B. Fildier, C. J. Muller, R. Pincus, and S. Fueglistaler, “How moisture shapes
    low‐level radiative cooling in subsidence regimes,” <i>AGU Advances</i>, vol.
    4, no. 3. American Geophysical Union, 2023.
  ista: Fildier B, Muller CJ, Pincus R, Fueglistaler S. 2023. How moisture shapes
    low‐level radiative cooling in subsidence regimes. AGU Advances. 4(3), e2023AV000880.
  mla: Fildier, B., et al. “How Moisture Shapes Low‐level Radiative Cooling in Subsidence
    Regimes.” <i>AGU Advances</i>, vol. 4, no. 3, e2023AV000880, American Geophysical
    Union, 2023, doi:<a href="https://doi.org/10.1029/2023av000880">10.1029/2023av000880</a>.
  short: B. Fildier, C.J. Muller, R. Pincus, S. Fueglistaler, AGU Advances 4 (2023).
date_created: 2024-01-08T13:07:49Z
date_published: 2023-06-01T00:00:00Z
date_updated: 2025-09-09T14:13:05Z
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doi: 10.1029/2023av000880
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title: How moisture shapes low‐level radiative cooling in subsidence regimes
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