---
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
PlanS_conform: '1'
_id: '21013'
abstract:
- lang: eng
text: We have addressed convective self‐aggregation (CSA) in steady and oscillating
sea surface temperature (SST) and solar radiation (SOLIN) cloud‐resolving model
simulations in a non‐rotating radiative‐convective equilibrium (RCE) framework.
Our experiment designs are motivated by land‐ocean heterogeneity of atmospheric
convection. The steady and oscillating forcings are idealizations of ocean and
land conditions, respectively, based on their differences in heat capacities.
In both kinds of simulations, the diurnal mean SST and SOLIN are the same, and
both SST and SOLIN are only varied in time (i.e., they are spatially homogeneous
at any given time). We find that diurnally oscillating forcing accelerates CSA.
Stronger long‐wave cooling in dry regions at night and during the warm SST phase
(late afternoon) both allow the long‐wave feedback, known to favor aggregation,
to intensify compared to steady forcing simulations. In addition to the long‐wave,
reduced short‐wave warming in dry regions (during the day) further enhances radiative
cooling there compared to moist regions. Overall, the radiative cooling is enhanced
in dry regions compared to neighboring moist convective regions. A dry subsidence
is driven by this net radiative (short‐wave plus long‐wave) cooling, consistent
with earlier work on CSA. Stronger radiative cooling allows stronger subsidence
which allows low‐level circulation to more efficiently transport moisture and
energy up‐gradient, driving convection to aggregate faster. We also note a sensitivity
of our experimental setup to initial conditions, more so at warmer SST. This stochastic
behavior might be critical in reconciling the differences of opinion regarding
the response of convection aggregation to oscillating SST forcing.
acknowledged_ssus:
- _id: ScienComp
acknowledgement: The authors 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). This research was supported by the
Scientific Service Units (SSU) of ISTA through resources provided by Scientific
Computing (SciComp). We are grateful to three anonymous reviewer(s) for their insightful
suggestions that have improved the quality of our manuscript. Open Access funding
provided by Institute of Science and Technology Austria/KEMÖ.
article_number: e2024MS004576
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
- first_name: Ziyin
full_name: Lu, Ziyin
id: a6e549c6-8972-11ed-ae7b-a336d97ac043
last_name: Lu
orcid: 0009-0008-5320-7730
- 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: GOSWAMI BB, Lu Z, Muller CJ. Convective self‐aggregation in diurnally oscillating
sea surface temperature and solar forcing experiments. Journal of Advances
in Modeling Earth Systems. 2026;18(1). doi:10.1029/2024ms004576
apa: GOSWAMI, B. B., Lu, Z., & Muller, C. J. (2026). Convective self‐aggregation
in diurnally oscillating sea surface temperature and solar forcing experiments.
Journal of Advances in Modeling Earth Systems. Wiley. https://doi.org/10.1029/2024ms004576
chicago: GOSWAMI, BIDYUT B, Ziyin Lu, and Caroline J Muller. “Convective Self‐aggregation
in Diurnally Oscillating Sea Surface Temperature and Solar Forcing Experiments.”
Journal of Advances in Modeling Earth Systems. Wiley, 2026. https://doi.org/10.1029/2024ms004576.
ieee: B. B. GOSWAMI, Z. Lu, and C. J. Muller, “Convective self‐aggregation in diurnally
oscillating sea surface temperature and solar forcing experiments,” Journal
of Advances in Modeling Earth Systems, vol. 18, no. 1. Wiley, 2026.
ista: GOSWAMI BB, Lu Z, Muller CJ. 2026. Convective self‐aggregation in diurnally
oscillating sea surface temperature and solar forcing experiments. Journal of
Advances in Modeling Earth Systems. 18(1), e2024MS004576.
mla: GOSWAMI, BIDYUT B., et al. “Convective Self‐aggregation in Diurnally Oscillating
Sea Surface Temperature and Solar Forcing Experiments.” Journal of Advances
in Modeling Earth Systems, vol. 18, no. 1, e2024MS004576, Wiley, 2026, doi:10.1029/2024ms004576.
short: B.B. GOSWAMI, Z. Lu, C.J. Muller, Journal of Advances in Modeling Earth Systems
18 (2026).
corr_author: '1'
date_created: 2026-01-20T10:08:54Z
date_published: 2026-01-12T00:00:00Z
date_updated: 2026-01-21T08:41:19Z
day: '12'
ddc:
- '550'
department:
- _id: CaMu
- _id: BjHo
- _id: GradSch
doi: 10.1029/2024ms004576
ec_funded: 1
file:
- access_level: open_access
checksum: 6ea369e3b46bea58efab4f38b6c671a7
content_type: application/pdf
creator: dernst
date_created: 2026-01-21T08:39:01Z
date_updated: 2026-01-21T08:39:01Z
file_id: '21027'
file_name: 2026_JAMES_Goswami.pdf
file_size: 19509786
relation: main_file
success: 1
file_date_updated: 2026-01-21T08:39:01Z
has_accepted_license: '1'
intvolume: ' 18'
issue: '1'
language:
- iso: eng
month: '01'
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: Convective self‐aggregation in diurnally oscillating sea surface temperature
and solar forcing experiments
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: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 18
year: '2026'
...
---
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '21657'
abstract:
- lang: eng
text: We compare three global kilometer-scale models (ICON, IFS and NICAM) to clarify
the advantages and challenges of high-resolution global weather and climate modeling,
using different approaches to represent convection, from fully parameterized to
fully explicit. Our analysis focuses on tropical precipitation characteristics
spanning a wide range of spatio-temporal scales—including the diurnal cycle, extreme
precipitation, convective organization, and the Madden-Julian Oscillation (MJO)—along
with interactions between convection and the thermodynamic environment. All three
models commonly show weaker convective organization with smaller precipitation
cells than observed, though the strength of the bias varies by model. This diversity
is introduced by differences in the representation of (a) convective initiation
affected by the convective sensitivity to moisture and (b) tropospheric moistening
associated with deep convection. Models with stronger thermodynamic-convection
coupling increase environmental moisture near convection, thereby enhancing convective
organization. This has important upscale effects on the MJO; while IFS and NICAM
capture its eastward propagation well, ICON has difficulty reproducing it. The
amplitudes and phases of precipitation diurnal cycles over land show much greater
disagreement among the models than over ocean, influenced by how convection is
initiated. Biases in rain evaporation and cold pool formation hinder the propagation
of mesoscale convection, leading to errors such as the misrepresentation of nocturnal
convection moving off the coast of Sumatra in IFS and ICON. These results highlight
the importance of thermodynamic-convection coupling in realistically simulating
tropical convection across scales. To improve this coupling, kilometer-scale models
require better representation of the interaction between resolved convection and
three-dimensional turbulent mixing.
acknowledgement: 'We thank Peter Bechtold, Lukas Brunner, Peter Dueben, Richard Forbes,
Estibaliz Gascon, and Benoit Vanniere for providing insightful comments on the present
study. We also thank Sebastian Milinski, Xabier Pedruzo and Thomas Rackow for their
contributions to setting up IFS-FESOM for nextGEMS. We are also grateful to Dr.
Walter Hannah and an anonymous reviewer for their constructive comments, which improved
the original version of the manuscript. D. Takasuka was supported by JSPS KAKENHI
Grants 20H05728 and 24K22893 and by JSPS Core-to-Core Program, “International Core-to-Core
Project on Global Storm Resolving Analysis” (Grant Number: JPJSCCA20220001). T.
Becker was supported by the Horizon 2020 project nextGEMS under grant agreement
number 101003470. J. Bao acknowledges funding from the European Union''s Horizon
2020 research and innovation programme under the Marie Skłodowska-Curie grant (grant
agreement No 101034413). The ICON and IFS simulations were performed with supercomputing
resources of the German Climate Computing Centre (Deutsches Klimarechenzentrum,
DKRZ) granted by its Scientific Steering Committee (WLA) under project ID 1235.
The NICAM simulation was performed on the supercomputer Fugaku (proposal numbers
hp220132, hp230078, hp230108, hp230278, and hp240267).'
article_number: e2025MS005343
article_processing_charge: Yes
article_type: original
author:
- first_name: Daisuke
full_name: Takasuka, Daisuke
last_name: Takasuka
- first_name: Tobias
full_name: Becker, Tobias
last_name: Becker
- first_name: Jiawei
full_name: Bao, Jiawei
id: bb9a7399-fefd-11ed-be3c-ae648fd1d160
last_name: Bao
citation:
ama: Takasuka D, Becker T, Bao J. Precipitation characteristics and thermodynamic-convection
coupling in global kilometer-scale simulations. Journal of Advances in Modeling
Earth Systems. 2026;18(3). doi:10.1029/2025MS005343
apa: Takasuka, D., Becker, T., & Bao, J. (2026). Precipitation characteristics
and thermodynamic-convection coupling in global kilometer-scale simulations. Journal
of Advances in Modeling Earth Systems. Wiley. https://doi.org/10.1029/2025MS005343
chicago: Takasuka, Daisuke, Tobias Becker, and Jiawei Bao. “Precipitation Characteristics
and Thermodynamic-Convection Coupling in Global Kilometer-Scale Simulations.”
Journal of Advances in Modeling Earth Systems. Wiley, 2026. https://doi.org/10.1029/2025MS005343.
ieee: D. Takasuka, T. Becker, and J. Bao, “Precipitation characteristics and thermodynamic-convection
coupling in global kilometer-scale simulations,” Journal of Advances in Modeling
Earth Systems, vol. 18, no. 3. Wiley, 2026.
ista: Takasuka D, Becker T, Bao J. 2026. Precipitation characteristics and thermodynamic-convection
coupling in global kilometer-scale simulations. Journal of Advances in Modeling
Earth Systems. 18(3), e2025MS005343.
mla: Takasuka, Daisuke, et al. “Precipitation Characteristics and Thermodynamic-Convection
Coupling in Global Kilometer-Scale Simulations.” Journal of Advances in Modeling
Earth Systems, vol. 18, no. 3, e2025MS005343, Wiley, 2026, doi:10.1029/2025MS005343.
short: D. Takasuka, T. Becker, J. Bao, Journal of Advances in Modeling Earth Systems
18 (2026).
corr_author: '1'
date_created: 2026-04-05T22:01:31Z
date_published: 2026-03-01T00:00:00Z
date_updated: 2026-06-16T10:43:35Z
day: '01'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2025MS005343
ec_funded: 1
file:
- access_level: open_access
checksum: ca7dac4bab31348d0640ed22580c6dce
content_type: application/pdf
creator: dernst
date_created: 2026-04-07T09:11:23Z
date_updated: 2026-04-07T09:11:23Z
file_id: '21665'
file_name: 2026_JAMES_Takasuka.pdf
file_size: 3854313
relation: main_file
success: 1
file_date_updated: 2026-04-07T09:11:23Z
has_accepted_license: '1'
intvolume: ' 18'
issue: '3'
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'
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: Precipitation characteristics and thermodynamic-convection coupling in global
kilometer-scale simulations
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: 18
year: '2026'
...
---
OA_place: publisher
OA_type: gold
_id: '19416'
abstract:
- lang: eng
text: 'Recently, Biagioli and Tompkins (2023, https://doi.org/10.1029/2022ms003231)
used a simple stochastic model to derive a dimensionless parameter to predict
convective self aggregation (SA) development, which was based on the derivation
of the maximum free convective distance ($d_{clr}$) expected in the pre-aggregated,
random state. Our goal is to test and further investigate this hypothesis, namely
that $d_{clr}$ can predict SA occurrence, using an ensemble of twenty-four distinct
combinations of horizontal mixing, planetary boundary layer (PBL), and microphysical
parameterizations. We conclude that the key impact of parameterization schemes
on SA is through their control of the number of convective cores and their relative
spacing, $d_{clr}$, which itself is impacted by cold-pool (CP) properties and
mean updraft core size. SA is more likely when the convective core count is small,
while CPs modify convective spacing via suppression in their interiors and triggering
by gust-front convergence and collisions. Each parameterization scheme emphasizes
a different mechanism. Subgrid-scale horizontal turbulent mixing mainly affects
SA through the determination of convective core size and thus spacing. The sensitivity
to the microphysics is mainly through rain evaporation and the subsequent impact
on CPs, while perturbations to the ice cloud microphysics have a limited effect.
Non-local PBL mixing schemes promote SA primarily by increasing convective inhibition
through inversion entrainment and altering low cloud amounts, leading to fewer
convective cores and larger $d_{clr}$. '
acknowledgement: This article is based on chapter 3 of AC Ph.D. thesis. The authors
thank Graziano Giuliani for his coding assistance. We also thank Daniel Hernández-Deckers,
Paolina Cerlini, and especially to Giovanni Biagioli for discussions and feedback.
We also thank two reviewers for their insightful comments. AC was supported by a
fellowship awarded by ICTP and by the European Union Horizon 2020 Marie Skłodowska-Curie
grant agreement No. 101034413. CM 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: e2024MS004791
article_processing_charge: Yes
article_type: original
author:
- first_name: Alejandro
full_name: Casallas Garcia, Alejandro
id: 92081129-2d75-11ef-a48d-b04dd7a2385a
last_name: Casallas Garcia
orcid: 0000-0002-1988-5035
- first_name: A.M.
full_name: Tompkins, A.M.
last_name: Tompkins
- 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: G.
full_name: Thompson, G.
last_name: Thompson
citation:
ama: Casallas Garcia A, Tompkins AM, Muller CJ, Thompson G. Sensitivity of self-aggregation
and the key role of the free convection distance. Journal of Advances in Modeling
Earth Systems. 2025;17(3). doi:10.1029/2024MS004791
apa: Casallas Garcia, A., Tompkins, A. M., Muller, C. J., & Thompson, G. (2025).
Sensitivity of self-aggregation and the key role of the free convection distance.
Journal of Advances in Modeling Earth Systems. Wiley. https://doi.org/10.1029/2024MS004791
chicago: Casallas Garcia, Alejandro, A.M. Tompkins, Caroline J Muller, and G. Thompson.
“Sensitivity of Self-Aggregation and the Key Role of the Free Convection Distance.”
Journal of Advances in Modeling Earth Systems. Wiley, 2025. https://doi.org/10.1029/2024MS004791.
ieee: A. Casallas Garcia, A. M. Tompkins, C. J. Muller, and G. Thompson, “Sensitivity
of self-aggregation and the key role of the free convection distance,” Journal
of Advances in Modeling Earth Systems, vol. 17, no. 3. Wiley, 2025.
ista: Casallas Garcia A, Tompkins AM, Muller CJ, Thompson G. 2025. Sensitivity of
self-aggregation and the key role of the free convection distance. Journal of
Advances in Modeling Earth Systems. 17(3), e2024MS004791.
mla: Casallas Garcia, Alejandro, et al. “Sensitivity of Self-Aggregation and the
Key Role of the Free Convection Distance.” Journal of Advances in Modeling
Earth Systems, vol. 17, no. 3, e2024MS004791, Wiley, 2025, doi:10.1029/2024MS004791.
short: A. Casallas Garcia, A.M. Tompkins, C.J. Muller, G. Thompson, Journal of Advances
in Modeling Earth Systems 17 (2025).
corr_author: '1'
date_created: 2025-03-19T07:58:38Z
date_published: 2025-03-18T00:00:00Z
date_updated: 2025-09-30T11:04:38Z
day: '18'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2024MS004791
ec_funded: 1
external_id:
isi:
- '001447023900001'
file:
- access_level: open_access
checksum: bc32677e63f8abb07b330f4a08da796d
content_type: application/pdf
creator: acasalla
date_created: 2025-03-19T07:58:21Z
date_updated: 2025-03-19T07:58:21Z
file_id: '19417'
file_name: Casallas_et_al_2025_dclr.pdf
file_size: 18285343
relation: main_file
file_date_updated: 2025-03-19T07:58:21Z
has_accepted_license: '1'
intvolume: ' 17'
isi: 1
issue: '3'
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: 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: Sensitivity of self-aggregation and the key role of the free convection distance
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: 17
year: '2025'
...
---
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. Journal
of Advances in Modeling Earth Systems. 2025;17(4). doi:10.1029/2024MS004613'
apa: 'Polesello, A., Charinti, G. A., Meroni, A. N., Muller, C. J., & Pasquero,
C. (2025). Intensity oscillations of tropical cyclones: Surface versus mid and
upper tropospheric processes. Journal of Advances in Modeling Earth Systems.
Wiley. https://doi.org/10.1029/2024MS004613'
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.” Journal of Advances in
Modeling Earth Systems. Wiley, 2025. https://doi.org/10.1029/2024MS004613.'
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,” Journal of Advances in Modeling Earth Systems, 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.” Journal of Advances in Modeling
Earth Systems, vol. 17, no. 4, e2024MS004613, Wiley, 2025, doi:10.1029/2024MS004613.'
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
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'
...
---
DOAJ_listed: '1'
OA_place: publisher
OA_type: gold
_id: '20319'
abstract:
- lang: eng
text: The time needed by deep convection to bring the atmosphere back to equilibrium
is called convective adjustment timescale or simply adjustment timescale, typically
denoted by . In the Community Atmospheric Model|Community Atmosphere Model (CAM), is
the convective available potential energy (CAPE) relaxation timescale and is 1 hr,
worldwide. Observational evidence suggests that is generally longer than 1 hr.
Further, continental and oceanic convection are different in terms of the vigor
of updrafts and can have different longevities. So using hour worldwide in CAM
has two potential caveats. A longer improves the simulation of the mean climate.
However, it does not address the land‐ocean heterogeneity of atmospheric deep
convection. We investigate the prescription of two different CAPE relaxation timescales
for land ( hr) and ocean ( to 4 hr). It is arguably an extremely crude parameterization
of boundary layer control on atmospheric convection. We contrast a suite of 5‐year‐long
simulations with two different for land and ocean to having one globally. The
choice of longer over ocean is guided by previous studies and inspired by observational
pieces of evidence. Nonetheless, to complement our variable experiments, we perform
a simulation with hr and hrs. Most importantly, our key findings are immune
to the exact values of prescribed and . The CAM model, with two values , improves
convective‐stratiform rainfall partitioning and the Madden–Julian oscillation
propagation characteristics.
acknowledged_ssus:
- _id: ScienComp
acknowledgement: The authors gratefully acknowledge funding from the European Research
Council (ERC) under the European Union's Horizon 2020 research and innovation program
(Project CLUSTER, Grant 805041). This research was supported by the Scientific Service
Units (SSU) of ISTA through resources provided by Scientific Computing (SciComp).
We would like to thank Prof. Courtney Schumacher and Dr. Aaron Funk of Texas A&M
University for their help in understanding the TRMM Radar data. The authors are
grateful to two anonymous reviewers who helped improve the quality of this paper.
article_number: e2025MS005035
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
- first_name: Andrea
full_name: Polesello, Andrea
id: 74c777f4-32da-11ee-b498-874db0835561
last_name: Polesello
- 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: GOSWAMI BB, Polesello A, Muller CJ. An assessment of representing land‐ocean
heterogeneity via CAPE relaxation timescale in the Community Atmospheric Model
6 (CAM6). Journal of Advances in Modeling Earth Systems. 2025;17(9). doi:10.1029/2025ms005035
apa: GOSWAMI, B. B., Polesello, A., & Muller, C. J. (2025). An assessment of
representing land‐ocean heterogeneity via CAPE relaxation timescale in the Community
Atmospheric Model 6 (CAM6). Journal of Advances in Modeling Earth Systems.
Wiley. https://doi.org/10.1029/2025ms005035
chicago: GOSWAMI, BIDYUT B, Andrea Polesello, and Caroline J Muller. “An Assessment
of Representing Land‐ocean Heterogeneity via CAPE Relaxation Timescale in the
Community Atmospheric Model 6 (CAM6).” Journal of Advances in Modeling Earth
Systems. Wiley, 2025. https://doi.org/10.1029/2025ms005035.
ieee: B. B. GOSWAMI, A. Polesello, and C. J. Muller, “An assessment of representing
land‐ocean heterogeneity via CAPE relaxation timescale in the Community Atmospheric
Model 6 (CAM6),” Journal of Advances in Modeling Earth Systems, vol. 17,
no. 9. Wiley, 2025.
ista: GOSWAMI BB, Polesello A, Muller CJ. 2025. An assessment of representing land‐ocean
heterogeneity via CAPE relaxation timescale in the Community Atmospheric Model
6 (CAM6). Journal of Advances in Modeling Earth Systems. 17(9), e2025MS005035.
mla: GOSWAMI, BIDYUT B., et al. “An Assessment of Representing Land‐ocean Heterogeneity
via CAPE Relaxation Timescale in the Community Atmospheric Model 6 (CAM6).” Journal
of Advances in Modeling Earth Systems, vol. 17, no. 9, e2025MS005035, Wiley,
2025, doi:10.1029/2025ms005035.
short: B.B. GOSWAMI, A. Polesello, C.J. Muller, Journal of Advances in Modeling
Earth Systems 17 (2025).
corr_author: '1'
date_created: 2025-09-10T05:36:16Z
date_published: 2025-09-01T00:00:00Z
date_updated: 2025-09-10T08:14:28Z
day: '01'
ddc:
- '550'
department:
- _id: CaMu
doi: 10.1029/2025ms005035
ec_funded: 1
file:
- access_level: open_access
checksum: 5961d6290432c5ac0e8587ef07f30c9b
content_type: application/pdf
creator: dernst
date_created: 2025-09-10T08:12:34Z
date_updated: 2025-09-10T08:12:34Z
file_id: '20338'
file_name: 2025_JAMES_Goswami.pdf
file_size: 2143025
relation: main_file
success: 1
file_date_updated: 2025-09-10T08:12:34Z
has_accepted_license: '1'
intvolume: ' 17'
issue: '9'
language:
- iso: eng
month: '09'
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: An assessment of representing land‐ocean heterogeneity via CAPE relaxation
timescale in the Community Atmospheric Model 6 (CAM6)
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: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 17
year: '2025'
...
---
_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.
Journal of Advances in Modeling Earth Systems. 2023;15(10). doi:10.1029/2022MS003477
apa: Abramian, S., Muller, C. J., & Risi, C. (2023). Extreme precipitation in
tropical squall lines. Journal of Advances in Modeling Earth Systems. Wiley.
https://doi.org/10.1029/2022MS003477
chicago: Abramian, Sophie, Caroline J Muller, and Camille Risi. “Extreme Precipitation
in Tropical Squall Lines.” Journal of Advances in Modeling Earth Systems.
Wiley, 2023. https://doi.org/10.1029/2022MS003477.
ieee: S. Abramian, C. J. Muller, and C. Risi, “Extreme precipitation in tropical
squall lines,” Journal of Advances in Modeling Earth Systems, 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.”
Journal of Advances in Modeling Earth Systems, vol. 15, no. 10, e2022MS003477,
Wiley, 2023, doi:10.1029/2022MS003477.
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:
- access_level: open_access
checksum: 43e6a1a35b663843c7d3f8d0caaca1a5
content_type: application/pdf
creator: dernst
date_created: 2023-10-30T13:31:42Z
date_updated: 2023-10-30T13:31:42Z
file_id: '14470'
file_name: 2023_JAMES_Abramian.pdf
file_size: 1975210
relation: main_file
success: 1
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:
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: 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.
Journal of Advances in Modeling Earth Systems. 2023;15(11). doi:10.1029/2022ms003391
apa: Khouider, B., GOSWAMI, B. B., Phani, R., & Majda, A. J. (2023). A shallow‐deep
unified stochastic mass flux cumulus parameterization in the single column community
climate model. Journal of Advances in Modeling Earth Systems. American
Geophysical Union. https://doi.org/10.1029/2022ms003391
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.” Journal of Advances in Modeling Earth Systems. American
Geophysical Union, 2023. https://doi.org/10.1029/2022ms003391.
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,” Journal of Advances in Modeling Earth Systems, 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.” Journal of Advances in Modeling
Earth Systems, vol. 15, no. 11, e2022MS003391, American Geophysical Union,
2023, doi:10.1029/2022ms003391.
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. Journal of Advances in Modeling Earth Systems.
2023;15(12). doi:10.1029/2023MS003726
apa: Hwong, Y.-L., Colin, M., Aglas, P., Muller, C. J., & Sherwood, S. C. (2023).
Assessing memory in convection schemes using idealized tests. Journal of Advances
in Modeling Earth Systems. Wiley. https://doi.org/10.1029/2023MS003726
chicago: Hwong, Yi-Ling, M. Colin, Philipp Aglas, Caroline J Muller, and S. C. Sherwood.
“Assessing Memory in Convection Schemes Using Idealized Tests.” Journal of
Advances in Modeling Earth Systems. Wiley, 2023. https://doi.org/10.1029/2023MS003726.
ieee: Y.-L. Hwong, M. Colin, P. Aglas, C. J. Muller, and S. C. Sherwood, “Assessing
memory in convection schemes using idealized tests,” Journal of Advances in
Modeling Earth Systems, 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.” Journal of Advances in Modeling Earth Systems, vol. 15, no. 12,
e2023MS003726, Wiley, 2023, doi:10.1029/2023MS003726.
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'
...