--- _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. Science Advances. 2024;10(8). doi:10.1126/sciadv.adj6801 apa: Bao, J., Stevens, B., Kluft, L., & Muller, C. J. (2024). Intensification of daily tropical precipitation extremes from more organized convection. Science Advances. American Association for the Advancement of Science. https://doi.org/10.1126/sciadv.adj6801 chicago: Bao, Jiawei, Bjorn Stevens, Lukas Kluft, and Caroline J Muller. “Intensification of Daily Tropical Precipitation Extremes from More Organized Convection.” Science Advances. American Association for the Advancement of Science, 2024. https://doi.org/10.1126/sciadv.adj6801. ieee: J. Bao, B. Stevens, L. Kluft, and C. J. Muller, “Intensification of daily tropical precipitation extremes from more organized convection,” Science Advances, 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.” Science Advances, vol. 10, no. 8, eadj6801, American Association for the Advancement of Science, 2024, doi:10.1126/sciadv.adj6801. 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: 2024-03-05T09:26:47Z day: '23' ddc: - '550' department: - _id: CaMu doi: 10.1126/sciadv.adj6801 ec_funded: 1 external_id: pmid: - '38394192' file: - access_level: open_access checksum: d4ec4f05a6d14745057e14d1b8bf45ae content_type: application/pdf creator: dernst date_created: 2024-03-04T07:34:00Z date_updated: 2024-03-04T07:34:00Z file_id: '15051' file_name: 2024_ScienceAdv_Bao.pdf file_size: 800926 relation: main_file success: 1 file_date_updated: 2024-03-04T07:34:00Z has_accepted_license: '1' intvolume: ' 10' issue: '8' language: - iso: eng 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 user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 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. Geoscientific Model Development. 2024;17(4):1563-1584. doi:10.5194/gmd-17-1563-2024 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. Geoscientific Model Development. European Geosciences Union. https://doi.org/10.5194/gmd-17-1563-2024 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.” Geoscientific Model Development. European Geosciences Union, 2024. https://doi.org/10.5194/gmd-17-1563-2024. ieee: H. Schmidt et al., “Effects of vertical grid spacing on the climate simulated in the ICON-Sapphire global storm-resolving model,” Geoscientific Model Development, 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.” Geoscientific Model Development, vol. 17, no. 4, European Geosciences Union, 2024, pp. 1563–84, doi:10.5194/gmd-17-1563-2024. 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: 2024-03-13T09:01:20Z day: '22' ddc: - '550' department: - _id: CaMu doi: 10.5194/gmd-17-1563-2024 file: - access_level: open_access checksum: 270d2340402729b0532f7072ea914cae content_type: application/pdf creator: dernst date_created: 2024-03-13T08:59:21Z date_updated: 2024-03-13T08:59:21Z file_id: '15111' file_name: 2024_GeoscientificModelDev_Schmidt.pdf file_size: 13364601 relation: main_file success: 1 file_date_updated: 2024-03-13T08:59:21Z has_accepted_license: '1' intvolume: ' 17' 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: 2DF688A6-F248-11E8-B48F-1D18A9856A87 volume: 17 year: '2024' ... --- _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 (in subscription journal) 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. Geophysical Research Letters. 2024;51(6). doi:10.1029/2023gl106523 apa: Hwong, Y.-L., & Muller, C. J. (2024). The unreasonable efficiency of total rain evaporation removal in triggering convective self‐aggregation. Geophysical Research Letters. American Geophysical Union. https://doi.org/10.1029/2023gl106523 chicago: Hwong, Yi-Ling, and Caroline J Muller. “The Unreasonable Efficiency of Total Rain Evaporation Removal in Triggering Convective Self‐aggregation.” Geophysical Research Letters. American Geophysical Union, 2024. https://doi.org/10.1029/2023gl106523. ieee: Y.-L. Hwong and C. J. Muller, “The unreasonable efficiency of total rain evaporation removal in triggering convective self‐aggregation,” Geophysical Research Letters, vol. 51, no. 6. American Geophysical Union, 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.” Geophysical Research Letters, vol. 51, no. 6, e2023GL106523, American Geophysical Union, 2024, doi:10.1029/2023gl106523. short: Y.-L. Hwong, C.J. Muller, Geophysical Research Letters 51 (2024). date_created: 2024-03-25T10:27:30Z date_published: 2024-03-19T00:00:00Z date_updated: 2024-03-25T11:32:06Z day: '19' ddc: - '550' department: - _id: CaMu doi: 10.1029/2023gl106523 ec_funded: 1 file: - access_level: open_access checksum: eacb011091a503b9e7b748fef639ba4c content_type: application/pdf 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' issue: '6' keyword: - General Earth and Planetary Sciences - Geophysics language: - iso: eng license: https://creativecommons.org/licenses/by-nc-nd/4.0/ 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: American Geophysical Union quality_controlled: '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: 2DF688A6-F248-11E8-B48F-1D18A9856A87 volume: 51 year: '2024' ... --- _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. Geophysical Research Letters. 2024;51(5). doi:10.1029/2023GL106569 apa: GOSWAMI, B. B. (2024). A pre-monsoon signal of false alarms of Indian monsoon droughts. Geophysical Research Letters. Wiley. https://doi.org/10.1029/2023GL106569 chicago: GOSWAMI, BIDYUT B. “A Pre-Monsoon Signal of False Alarms of Indian Monsoon Droughts.” Geophysical Research Letters. Wiley, 2024. https://doi.org/10.1029/2023GL106569. ieee: B. B. GOSWAMI, “A pre-monsoon signal of false alarms of Indian monsoon droughts,” Geophysical Research Letters, 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.” Geophysical Research Letters, vol. 51, no. 5, e2023GL106569, Wiley, 2024, doi:10.1029/2023GL106569. short: B.B. GOSWAMI, Geophysical Research Letters 51 (2024). date_created: 2024-03-24T23:00:58Z date_published: 2024-03-16T00:00:00Z date_updated: 2024-03-25T10:00:57Z day: '16' ddc: - '550' department: - _id: CaMu doi: 10.1029/2023GL106569 ec_funded: 1 file: - access_level: open_access checksum: 243bd966aca968ec7d9e474af8639f8d 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' 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: 2DF688A6-F248-11E8-B48F-1D18A9856A87 volume: 51 year: '2024' ... --- _id: '11434' abstract: - lang: eng text: The Indian summer monsoon rainfall (ISMR) has been declining since the 1950s. However, since 2002 it is reported to have revived. For these observed changes in the ISMR, several explanations have been reported. Among these explanations, however, the role of the eastern equatorial Indian Ocean (EEIO) is missing despite being one of the warmest regions in the Indian Ocean, and monotonously warming. A recent study reported that EEIO warming impacts the rainfall over northern India. Here we report that warming in the EEIO weakens the low-level Indian summer monsoon circulation and reduces ISMR. A warm EEIO drives easterly winds in the Indo–Pacific sector as a Gill response. The warm EEIO also enhances nocturnal convection offshore the western coast of Sumatra. The latent heating associated with the increased convection augments the Gill response and the resultant circulation opposes the monsoon low-level circulation and weakens the seasonal rainfall. acknowledgement: This work was supported by the National Research Foundation of Korea (NRF) grant funded by the Korea government (MSIT) (NRF-2018R1A5A1024958). 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 Korea Meteorological Administration, and by the Korea Research Environment Open NETwork (KREONET), respectively. The authors declare no conflicts of interest. article_processing_charge: No article_type: original author: - first_name: Bidyut B full_name: Goswami, Bidyut B id: 3a4ac09c-6d61-11ec-bf66-884cde66b64b last_name: Goswami citation: ama: GOSWAMI BB. Role of the eastern equatorial Indian Ocean warming in the Indian summer monsoon rainfall trend. Climate Dynamics. 2023;60:427-442. doi:10.1007/s00382-022-06337-7 apa: GOSWAMI, B. B. (2023). Role of the eastern equatorial Indian Ocean warming in the Indian summer monsoon rainfall trend. Climate Dynamics. Springer Nature. https://doi.org/10.1007/s00382-022-06337-7 chicago: GOSWAMI, BIDYUT B. “Role of the Eastern Equatorial Indian Ocean Warming in the Indian Summer Monsoon Rainfall Trend.” Climate Dynamics. Springer Nature, 2023. https://doi.org/10.1007/s00382-022-06337-7. ieee: B. B. GOSWAMI, “Role of the eastern equatorial Indian Ocean warming in the Indian summer monsoon rainfall trend,” Climate Dynamics, vol. 60. Springer Nature, pp. 427–442, 2023. ista: GOSWAMI BB. 2023. Role of the eastern equatorial Indian Ocean warming in the Indian summer monsoon rainfall trend. Climate Dynamics. 60, 427–442. mla: GOSWAMI, BIDYUT B. “Role of the Eastern Equatorial Indian Ocean Warming in the Indian Summer Monsoon Rainfall Trend.” Climate Dynamics, vol. 60, Springer Nature, 2023, pp. 427–42, doi:10.1007/s00382-022-06337-7. short: B.B. GOSWAMI, Climate Dynamics 60 (2023) 427–442. date_created: 2022-06-05T22:01:50Z date_published: 2023-01-01T00:00:00Z date_updated: 2023-06-28T11:49:58Z day: '01' department: - _id: CaMu doi: 10.1007/s00382-022-06337-7 external_id: isi: - '000803119400002' intvolume: ' 60' isi: 1 language: - iso: eng month: '01' oa_version: None page: 427-442 publication: Climate Dynamics publication_identifier: eissn: - 1432-0894 issn: - 0930-7575 publication_status: published publisher: Springer Nature quality_controlled: '1' related_material: link: - relation: erratum url: ' https://doi.org/10.1007/s00382-022-06401-2' scopus_import: '1' status: public title: Role of the eastern equatorial Indian Ocean warming in the Indian summer monsoon rainfall trend type: journal_article user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 volume: 60 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 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. The European Physical Journal E. 2023;46(3). doi:10.1140/epje/s10189-023-00276-9 apa: Clark Di Leoni, P., Agasthya, L. N., Buzzicotti, M., & Biferale, L. (2023). Reconstructing Rayleigh–Bénard flows out of temperature-only measurements using Physics-Informed Neural Networks. The European Physical Journal E. Springer Nature. https://doi.org/10.1140/epje/s10189-023-00276-9 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.” The European Physical Journal E. Springer Nature, 2023. https://doi.org/10.1140/epje/s10189-023-00276-9. 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,” The European Physical Journal E, 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.” The European Physical Journal E, vol. 46, no. 3, 16, Springer Nature, 2023, doi:10.1140/epje/s10189-023-00276-9. 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: 2023-08-01T14:03:47Z day: '20' department: - _id: CaMu doi: 10.1140/epje/s10189-023-00276-9 external_id: arxiv: - '2301.07769' isi: - '000956387200001' 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 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: 4359f0d1-fa6c-11eb-b949-802e58b17ae8 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. npj Climate and Atmospheric Science. 2023;6. doi:10.1038/s41612-023-00411-5 apa: GOSWAMI, B. B., & An, S. I. (2023). An assessment of the ENSO-monsoon teleconnection in a warming climate. Npj Climate and Atmospheric Science. Springer Nature. https://doi.org/10.1038/s41612-023-00411-5 chicago: GOSWAMI, BIDYUT B, and Soon Il An. “An Assessment of the ENSO-Monsoon Teleconnection in a Warming Climate.” Npj Climate and Atmospheric Science. Springer Nature, 2023. https://doi.org/10.1038/s41612-023-00411-5. ieee: B. B. GOSWAMI and S. I. An, “An assessment of the ENSO-monsoon teleconnection in a warming climate,” npj Climate and Atmospheric Science, 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.” Npj Climate and Atmospheric Science, vol. 6, 82, Springer Nature, 2023, doi:10.1038/s41612-023-00411-5. 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: '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: 2023-11-28T12:04:42Z day: '01' ddc: - '550' department: - _id: CaMu doi: 10.1029/2022ms003391 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' issue: '11' keyword: - General Earth and Planetary Sciences - Environmental Chemistry - Global and Planetary Change language: - iso: eng license: https://creativecommons.org/licenses/by-nc/4.0/ 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: 2DF688A6-F248-11E8-B48F-1D18A9856A87 volume: 15 year: '2023' ... --- _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: 2023-12-13T13:06:40Z 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: '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. AGU Advances. 2023;4(3). doi:10.1029/2023av000880 apa: Fildier, B., Muller, C. J., Pincus, R., & Fueglistaler, S. (2023). How moisture shapes low‐level radiative cooling in subsidence regimes. AGU Advances. American Geophysical Union. https://doi.org/10.1029/2023av000880 chicago: Fildier, B., Caroline J Muller, R. Pincus, and S. Fueglistaler. “How Moisture Shapes Low‐level Radiative Cooling in Subsidence Regimes.” AGU Advances. American Geophysical Union, 2023. https://doi.org/10.1029/2023av000880. ieee: B. Fildier, C. J. Muller, R. Pincus, and S. Fueglistaler, “How moisture shapes low‐level radiative cooling in subsidence regimes,” AGU Advances, 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.” AGU Advances, vol. 4, no. 3, e2023AV000880, American Geophysical Union, 2023, doi:10.1029/2023av000880. 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: 2024-01-09T08:54:03Z day: '01' ddc: - '550' department: - _id: CaMu doi: 10.1029/2023av000880 ec_funded: 1 file: - access_level: open_access checksum: af773220a9fa194c61a8dc2fae092c16 content_type: application/pdf creator: dernst date_created: 2024-01-09T08:51:25Z date_updated: 2024-01-09T08:51:25Z file_id: '14761' file_name: 2023_AGUAdvances_Fildier.pdf file_size: 24149551 relation: main_file success: 1 file_date_updated: 2024-01-09T08:51:25Z has_accepted_license: '1' intvolume: ' 4' issue: '3' keyword: - General Earth and Planetary Sciences language: - iso: eng month: '06' 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: AGU Advances publication_identifier: eissn: - 2576-604X publication_status: published publisher: American Geophysical Union quality_controlled: '1' scopus_import: '1' status: public title: How moisture shapes low‐level radiative cooling in subsidence regimes 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: 4 year: '2023' ... --- _id: '14773' abstract: - lang: eng text: Through a combination of idealized simulations and real-world data, researchers are uncovering how internal feedbacks and large-scale motions influence cloud dynamics. article_number: '28' article_processing_charge: No article_type: original author: - 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: Sophie full_name: Abramian, Sophie last_name: Abramian citation: ama: Muller CJ, Abramian S. The cloud dynamics of convective storm systems. Physics Today. 2023;76(5). doi:10.1063/pt.3.5234 apa: Muller, C. J., & Abramian, S. (2023). The cloud dynamics of convective storm systems. Physics Today. AIP Publishing. https://doi.org/10.1063/pt.3.5234 chicago: Muller, Caroline J, and Sophie Abramian. “The Cloud Dynamics of Convective Storm Systems.” Physics Today. AIP Publishing, 2023. https://doi.org/10.1063/pt.3.5234. ieee: C. J. Muller and S. Abramian, “The cloud dynamics of convective storm systems,” Physics Today, vol. 76, no. 5. AIP Publishing, 2023. ista: Muller CJ, Abramian S. 2023. The cloud dynamics of convective storm systems. Physics Today. 76(5), 28. mla: Muller, Caroline J., and Sophie Abramian. “The Cloud Dynamics of Convective Storm Systems.” Physics Today, vol. 76, no. 5, 28, AIP Publishing, 2023, doi:10.1063/pt.3.5234. short: C.J. Muller, S. Abramian, Physics Today 76 (2023). date_created: 2024-01-10T09:18:04Z date_published: 2023-05-01T00:00:00Z date_updated: 2024-01-10T12:38:02Z day: '01' department: - _id: CaMu doi: 10.1063/pt.3.5234 external_id: isi: - '000984516100007' intvolume: ' 76' isi: 1 issue: '5' keyword: - General Physics and Astronomy language: - iso: eng main_file_link: - open_access: '1' url: https://www.lmd.ens.fr/muller/Pubs/2023-MullerAbramianPhysToday.pdf month: '05' oa: 1 oa_version: Published Version publication: Physics Today publication_identifier: eissn: - 1945-0699 issn: - 0031-9228 publication_status: published publisher: AIP Publishing quality_controlled: '1' status: public title: The cloud dynamics of convective storm systems type: journal_article user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 volume: 76 year: '2023' ... --- _id: '14853' abstract: - lang: eng text: Organization – or departure from a random pattern – in tropical deep convection is heavily studied due to its immediate relevance to climate sensitivity and extremes. Low-latitude convection has motivated numerical model idealizations, where the Coriolis force is removed and boundary conditions are simplified spatially and temporally. One of the most stunning aspects of such idealized simulated cloud organization is the spontaneous clumping of convection that can occur without any predetermining external perturbation, such as inhomogeneous surface boundary conditions or large-scale waves. Whereas individual convective rain cells measure only few kilometers in horizontal diameter, the clusters they form can often span hundreds or even thousands of kilometers. Hence, organization may emerge from the very small scales but can show effects at the synoptic scale. We refer to such emergent organization as convective self-organization. Convective self-organization thus features characteristics of emergence, such as non-trivial system-scale pattern formation or hysteresis. We summarize observational evidence for large-scale organization and briefly recap classical idealized modeling studies that yield convective self-aggregation – emergent organization under strongly idealized boundary conditions. We then focus on developing research, where temporal variation, such as the diurnal cycle, or two-way interactive surface properties yield distinct organizational modes. Convectively generated cold pools and mesoscale convective systems, both ubiquitous in nature, are thereby found to potentially play key roles in promoting – rather than suppressing – sustained system-scale organization. alternative_title: - Geophysical Monograph Series article_processing_charge: No author: - first_name: Jan O. full_name: Haerter, Jan O. last_name: Haerter - 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: 'Haerter JO, Muller CJ. Mechanisms for the Self‐Organization of Tropical Deep Convection. In: Sullivan S, Hoose C, eds. Clouds and Their Climatic Impacts. Wiley; 2023:179-193. doi:10.1002/9781119700357.ch8' apa: Haerter, J. O., & Muller, C. J. (2023). Mechanisms for the Self‐Organization of Tropical Deep Convection. In S. Sullivan & C. Hoose (Eds.), Clouds and Their Climatic Impacts (pp. 179–193). Wiley. https://doi.org/10.1002/9781119700357.ch8 chicago: Haerter, Jan O., and Caroline J Muller. “Mechanisms for the Self‐Organization of Tropical Deep Convection.” In Clouds and Their Climatic Impacts, edited by Sylvia Sullivan and Corinna Hoose, 179–93. Wiley, 2023. https://doi.org/10.1002/9781119700357.ch8. ieee: J. O. Haerter and C. J. Muller, “Mechanisms for the Self‐Organization of Tropical Deep Convection,” in Clouds and Their Climatic Impacts, S. Sullivan and C. Hoose, Eds. Wiley, 2023, pp. 179–193. ista: 'Haerter JO, Muller CJ. 2023.Mechanisms for the Self‐Organization of Tropical Deep Convection. In: Clouds and Their Climatic Impacts. Geophysical Monograph Series, , 179–193.' mla: Haerter, Jan O., and Caroline J. Muller. “Mechanisms for the Self‐Organization of Tropical Deep Convection.” Clouds and Their Climatic Impacts, edited by Sylvia Sullivan and Corinna Hoose, Wiley, 2023, pp. 179–93, doi:10.1002/9781119700357.ch8. short: J.O. Haerter, C.J. Muller, in:, S. Sullivan, C. Hoose (Eds.), Clouds and Their Climatic Impacts, Wiley, 2023, pp. 179–193. date_created: 2024-01-22T08:23:16Z date_published: 2023-12-15T00:00:00Z date_updated: 2024-01-23T12:40:36Z day: '15' department: - _id: CaMu doi: 10.1002/9781119700357.ch8 editor: - first_name: Sylvia full_name: Sullivan, Sylvia last_name: Sullivan - first_name: Corinna full_name: Hoose, Corinna last_name: Hoose language: - iso: eng month: '12' oa_version: None page: 179-193 publication: Clouds and Their Climatic Impacts publication_identifier: eisbn: - '9781119700357' isbn: - '9781119700319' issn: - 2328-8779 publication_status: published publisher: Wiley quality_controlled: '1' status: public title: Mechanisms for the Self‐Organization of Tropical Deep Convection type: book_chapter user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 year: '2023' ... --- _id: '14864' acknowledgement: This project has received funding from the European Research Council (ERC) under the European Union’s Starting Grant (No. 949120). article_number: '6166' article_processing_charge: No 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: 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, Muller CJ, Waitukaitis SR. Measuring spontaneous charging of single aerosol particles. In: EGU General Assembly 2023. European Geosciences Union; 2023. doi:10.5194/egusphere-egu23-6166' apa: 'Stöllner, A., Lenton, I. C., Muller, C. J., & Waitukaitis, S. R. (2023). Measuring spontaneous charging of single aerosol particles. In EGU General Assembly 2023. Vienna, Austria & Virtual: European Geosciences Union. https://doi.org/10.5194/egusphere-egu23-6166' chicago: Stöllner, Andrea, Isaac C Lenton, Caroline J Muller, and Scott R Waitukaitis. “Measuring Spontaneous Charging of Single Aerosol Particles.” In EGU General Assembly 2023. European Geosciences Union, 2023. https://doi.org/10.5194/egusphere-egu23-6166. ieee: A. Stöllner, I. C. Lenton, C. J. Muller, and S. R. Waitukaitis, “Measuring spontaneous charging of single aerosol particles,” in EGU General Assembly 2023, Vienna, Austria & Virtual, 2023. ista: Stöllner A, Lenton IC, Muller CJ, Waitukaitis SR. 2023. Measuring spontaneous charging of single aerosol particles. EGU General Assembly 2023. EGU General Assembly, 6166. mla: Stöllner, Andrea, et al. “Measuring Spontaneous Charging of Single Aerosol Particles.” EGU General Assembly 2023, 6166, European Geosciences Union, 2023, doi:10.5194/egusphere-egu23-6166. short: A. Stöllner, I.C. Lenton, C.J. Muller, S.R. Waitukaitis, in:, EGU General Assembly 2023, European Geosciences Union, 2023. conference: end_date: 2023-04-28 location: Vienna, Austria & Virtual name: EGU General Assembly start_date: 2023-04-23 date_created: 2024-01-22T12:09:07Z date_published: 2023-04-23T00:00:00Z date_updated: 2024-01-24T11:21:42Z day: '23' ddc: - '530' department: - _id: CaMu - _id: ScWa doi: 10.5194/egusphere-egu23-6166 ec_funded: 1 file: - access_level: open_access checksum: 8d6ddbb359e584b156f991f00196d86b content_type: application/pdf creator: dernst date_created: 2024-01-23T13:00:26Z date_updated: 2024-01-23T13:00:26Z file_id: '14880' file_name: 2023_EGU_Stoellner.pdf file_size: 419736 relation: main_file success: 1 file_date_updated: 2024-01-23T13:00:26Z has_accepted_license: '1' language: - iso: eng month: '04' 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' publication: EGU General Assembly 2023 publication_status: published publisher: European Geosciences Union status: public title: Measuring spontaneous charging of single aerosol particles 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_abstract user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 year: '2023' ... --- _id: '14863' article_number: EGU23-6157 article_processing_charge: No author: - 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 - first_name: Claudia full_name: Pasquero, Claudia last_name: Pasquero - first_name: Agostino N. full_name: Meroni, Agostino N. last_name: Meroni citation: ama: 'Polesello A, Muller CJ, Pasquero C, Meroni AN. Intensification mechanisms of tropical cyclones. In: EGU General Assembly 2023. European Geosciences Union; 2023. doi:10.5194/egusphere-egu23-6157' apa: 'Polesello, A., Muller, C. J., Pasquero, C., & Meroni, A. N. (2023). Intensification mechanisms of tropical cyclones. In EGU General Assembly 2023. Vienna, Austria & Virtual: European Geosciences Union. https://doi.org/10.5194/egusphere-egu23-6157' chicago: Polesello, Andrea, Caroline J Muller, Claudia Pasquero, and Agostino N. Meroni. “Intensification Mechanisms of Tropical Cyclones.” In EGU General Assembly 2023. European Geosciences Union, 2023. https://doi.org/10.5194/egusphere-egu23-6157. ieee: A. Polesello, C. J. Muller, C. Pasquero, and A. N. Meroni, “Intensification mechanisms of tropical cyclones,” in EGU General Assembly 2023, Vienna, Austria & Virtual, 2023. ista: Polesello A, Muller CJ, Pasquero C, Meroni AN. 2023. Intensification mechanisms of tropical cyclones. EGU General Assembly 2023. EGU General Assembly, EGU23-6157. mla: Polesello, Andrea, et al. “Intensification Mechanisms of Tropical Cyclones.” EGU General Assembly 2023, EGU23-6157, European Geosciences Union, 2023, doi:10.5194/egusphere-egu23-6157. short: A. Polesello, C.J. Muller, C. Pasquero, A.N. Meroni, in:, EGU General Assembly 2023, European Geosciences Union, 2023. conference: end_date: 2023-04-28 location: Vienna, Austria & Virtual name: EGU General Assembly start_date: 2023-04-23 date_created: 2024-01-22T12:08:12Z date_published: 2023-04-13T00:00:00Z date_updated: 2024-01-24T11:25:07Z day: '13' ddc: - '550' department: - _id: CaMu - _id: GradSch doi: 10.5194/egusphere-egu23-6157 file: - access_level: open_access checksum: 8cb88c1bc80ccee328478a62064d98f7 content_type: application/pdf creator: dernst date_created: 2024-01-24T11:19:54Z date_updated: 2024-01-24T11:19:54Z file_id: '14883' file_name: 2023_EGU_Polesello.pdf file_size: 296769 relation: main_file success: 1 file_date_updated: 2024-01-24T11:19:54Z has_accepted_license: '1' language: - iso: eng month: '04' oa: 1 oa_version: Published Version publication: EGU General Assembly 2023 publication_status: published publisher: European Geosciences Union status: public title: Intensification mechanisms of tropical cyclones 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_abstract user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 year: '2023' ... --- _id: '14865' article_number: EGU23-4968 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: Maxime full_name: Colin, Maxime 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: Steven full_name: Sherwood, Steven last_name: Sherwood citation: ama: 'Hwong Y-L, Colin M, Aglas P, Muller CJ, Sherwood S. Evaluating memory properties in convection schemes using idealised tests. In: EGU General Assembly 2023. European Geosciences Union; 2023. doi:10.5194/egusphere-egu23-4968' apa: 'Hwong, Y.-L., Colin, M., Aglas, P., Muller, C. J., & Sherwood, S. (2023). Evaluating memory properties in convection schemes using idealised tests. In EGU General Assembly 2023. Vienna, Austria & Virtual: European Geosciences Union. https://doi.org/10.5194/egusphere-egu23-4968' chicago: Hwong, Yi-Ling, Maxime Colin, Philipp Aglas, Caroline J Muller, and Steven Sherwood. “Evaluating Memory Properties in Convection Schemes Using Idealised Tests.” In EGU General Assembly 2023. European Geosciences Union, 2023. https://doi.org/10.5194/egusphere-egu23-4968. ieee: Y.-L. Hwong, M. Colin, P. Aglas, C. J. Muller, and S. Sherwood, “Evaluating memory properties in convection schemes using idealised tests,” in EGU General Assembly 2023, Vienna, Austria & Virtual, 2023. ista: Hwong Y-L, Colin M, Aglas P, Muller CJ, Sherwood S. 2023. Evaluating memory properties in convection schemes using idealised tests. EGU General Assembly 2023. EGU General Assembly, EGU23-4968. mla: Hwong, Yi-Ling, et al. “Evaluating Memory Properties in Convection Schemes Using Idealised Tests.” EGU General Assembly 2023, EGU23-4968, European Geosciences Union, 2023, doi:10.5194/egusphere-egu23-4968. short: Y.-L. Hwong, M. Colin, P. Aglas, C.J. Muller, S. Sherwood, in:, EGU General Assembly 2023, European Geosciences Union, 2023. conference: end_date: 2023-04-28 location: Vienna, Austria & Virtual name: EGU General Assembly start_date: 2023-04-23 date_created: 2024-01-22T12:10:32Z date_published: 2023-04-23T00:00:00Z date_updated: 2024-02-05T08:49:49Z day: '23' ddc: - '550' department: - _id: CaMu doi: 10.5194/egusphere-egu23-4968 file: - access_level: open_access checksum: 628a27caff437855ab320be46b9e8dcc content_type: application/pdf creator: dernst date_created: 2024-02-05T08:48:41Z date_updated: 2024-02-05T08:48:41Z file_id: '14936' file_name: 2023_EGU_Hwong.pdf file_size: 317541 relation: main_file success: 1 file_date_updated: 2024-02-05T08:48:41Z has_accepted_license: '1' language: - iso: eng month: '04' oa: 1 oa_version: Published Version publication: EGU General Assembly 2023 publication_status: published publisher: European Geosciences Union status: public title: Evaluating memory properties in convection schemes using idealised tests 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_abstract user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 year: '2023' ... --- _id: '14866' article_number: EGU23-15870 article_processing_charge: No 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. In: EGU General Assembly 2023. European Geosciences Union; 2023. doi:10.5194/egusphere-egu23-15870' apa: 'Abramian, S., Muller, C. J., & Risi, C. (2023). Extreme precipitation in tropical squall lines. In EGU General Assembly 2023. Vienna, Austria & Virtual: European Geosciences Union. https://doi.org/10.5194/egusphere-egu23-15870' chicago: Abramian, Sophie, Caroline J Muller, and Camille Risi. “Extreme Precipitation in Tropical Squall Lines.” In EGU General Assembly 2023. European Geosciences Union, 2023. https://doi.org/10.5194/egusphere-egu23-15870. ieee: S. Abramian, C. J. Muller, and C. Risi, “Extreme precipitation in tropical squall lines,” in EGU General Assembly 2023, Vienna, Austria & Virtual, 2023. ista: Abramian S, Muller CJ, Risi C. 2023. Extreme precipitation in tropical squall lines. EGU General Assembly 2023. EGU General Assembly, EGU23-15870. mla: Abramian, Sophie, et al. “Extreme Precipitation in Tropical Squall Lines.” EGU General Assembly 2023, EGU23-15870, European Geosciences Union, 2023, doi:10.5194/egusphere-egu23-15870. short: S. Abramian, C.J. Muller, C. Risi, in:, EGU General Assembly 2023, European Geosciences Union, 2023. conference: end_date: 2023-04-28 location: Vienna, Austria & Virtual name: EGU General Assembly start_date: 2023-04-23 date_created: 2024-01-22T12:10:52Z date_published: 2023-04-23T00:00:00Z date_updated: 2024-02-05T08:13:12Z day: '23' ddc: - '550' department: - _id: CaMu doi: 10.5194/egusphere-egu23-15870 file: - access_level: open_access checksum: 8cd5bb8bf3d48ceefb395b6875819147 content_type: application/pdf creator: dernst date_created: 2024-02-05T08:10:43Z date_updated: 2024-02-05T08:10:43Z file_id: '14935' file_name: 2023_EGU_Abramian.pdf file_size: 294690 relation: main_file success: 1 file_date_updated: 2024-02-05T08:10:43Z has_accepted_license: '1' language: - iso: eng month: '04' oa: 1 oa_version: Published Version publication: EGU General Assembly 2023 publication_status: published publisher: European Geosciences Union 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: conference_abstract user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 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). date_created: 2023-12-10T23:00:57Z date_published: 2023-12-01T00:00:00Z date_updated: 2024-02-27T07:26:30Z day: '01' ddc: - '550' department: - _id: CaMu doi: 10.1029/2023MS003726 ec_funded: 1 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' 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: 2DF688A6-F248-11E8-B48F-1D18A9856A87 volume: 15 year: '2023' ... --- _id: '14991' abstract: - lang: eng text: This repository contains the data, scripts, WRF codes and files required to reproduce the results of the manuscript "Assessing Memory in Convection Schemes Using Idealized Tests" submitted to the Journal of Advances in Modeling Earth Systems (JAMES). 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: Maxime full_name: Colin, Maxime 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: Steven C. full_name: Sherwood, Steven C. last_name: Sherwood citation: ama: Hwong Y-L, Colin M, Aglas P, Muller CJ, Sherwood SC. Data-assessing memory in convection schemes using idealized tests. 2023. doi:10.5281/ZENODO.7757041 apa: Hwong, Y.-L., Colin, M., Aglas, P., Muller, C. J., & Sherwood, S. C. (2023). Data-assessing memory in convection schemes using idealized tests. Zenodo. https://doi.org/10.5281/ZENODO.7757041 chicago: Hwong, Yi-Ling, Maxime Colin, Philipp Aglas, Caroline J Muller, and Steven C. Sherwood. “Data-Assessing Memory in Convection Schemes Using Idealized Tests.” Zenodo, 2023. https://doi.org/10.5281/ZENODO.7757041. ieee: Y.-L. Hwong, M. Colin, P. Aglas, C. J. Muller, and S. C. Sherwood, “Data-assessing memory in convection schemes using idealized tests.” Zenodo, 2023. ista: Hwong Y-L, Colin M, Aglas P, Muller CJ, Sherwood SC. 2023. Data-assessing memory in convection schemes using idealized tests, Zenodo, 10.5281/ZENODO.7757041. mla: Hwong, Yi-Ling, et al. Data-Assessing Memory in Convection Schemes Using Idealized Tests. Zenodo, 2023, doi:10.5281/ZENODO.7757041. short: Y.-L. Hwong, M. Colin, P. Aglas, C.J. Muller, S.C. Sherwood, (2023). date_created: 2024-02-14T14:37:57Z date_published: 2023-06-23T00:00:00Z date_updated: 2024-02-27T07:26:31Z day: '23' ddc: - '550' department: - _id: CaMu doi: 10.5281/ZENODO.7757041 ec_funded: 1 has_accepted_license: '1' main_file_link: - open_access: '1' url: https://doi.org/10.5281/zenodo.7757041 month: '06' 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' publisher: Zenodo related_material: record: - id: '14654' relation: used_in_publication status: public status: public title: Data-assessing memory in convection schemes using idealized tests 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: '2023' ... --- _id: '10653' abstract: - lang: eng text: Squall lines are known to be the consequence of the interaction of low-level shear with cold pools associated with convective downdrafts. Also, as the magnitude of the shear increases beyond a critical shear, squall lines tend to orient themselves. The existing literature suggests that this orientation reduces incoming wind shear to the squall line, and maintains equilibrium between wind shear and cold pool spreading. Although this theory is widely accepted, very few quantitative studies have been conducted on supercritical regime especially. Here, we test this hypothesis with tropical squall lines obtained by imposing a vertical wind shear in cloud resolving simulations in radiative convective equilibrium. In the sub-critical regime, squall lines are perpendicular to the shear. In the super-critical regime, their orientation maintain the equilibrium, supporting existing theories. We also find that as shear increases, cold pools become more intense. However, this intensification has little impact on squall line orientation. 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), and from the PhD fellowship of Ecole Normale Supérieure de Paris-Saclay. Two supplementary movies are also provided showing the angle detection method and the squall line of the Usfc = 10 m s−1 simulation. article_number: e2021GL095184 article_processing_charge: No 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. Shear-convection interactions and orientation of tropical squall lines. Geophysical Research Letters. 2022;49(1). doi:10.1029/2021GL095184 apa: Abramian, S., Muller, C. J., & Risi, C. (2022). Shear-convection interactions and orientation of tropical squall lines. Geophysical Research Letters. Wiley. https://doi.org/10.1029/2021GL095184 chicago: Abramian, Sophie, Caroline J Muller, and Camille Risi. “Shear-Convection Interactions and Orientation of Tropical Squall Lines.” Geophysical Research Letters. Wiley, 2022. https://doi.org/10.1029/2021GL095184. ieee: S. Abramian, C. J. Muller, and C. Risi, “Shear-convection interactions and orientation of tropical squall lines,” Geophysical Research Letters, vol. 49, no. 1. Wiley, 2022. ista: Abramian S, Muller CJ, Risi C. 2022. Shear-convection interactions and orientation of tropical squall lines. Geophysical Research Letters. 49(1), e2021GL095184. mla: Abramian, Sophie, et al. “Shear-Convection Interactions and Orientation of Tropical Squall Lines.” Geophysical Research Letters, vol. 49, no. 1, e2021GL095184, Wiley, 2022, doi:10.1029/2021GL095184. short: S. Abramian, C.J. Muller, C. Risi, Geophysical Research Letters 49 (2022). date_created: 2022-01-23T23:01:27Z date_published: 2022-01-16T00:00:00Z date_updated: 2023-08-02T14:00:17Z day: '16' ddc: - '550' department: - _id: CaMu doi: 10.1029/2021GL095184 ec_funded: 1 external_id: isi: - '000743989800040' file: - access_level: open_access checksum: 08f88b57b8e409b42e382452cd5f297b content_type: application/pdf creator: cchlebak date_created: 2022-01-24T12:14:41Z date_updated: 2022-01-24T12:14:41Z file_id: '10662' file_name: 2022_GeophysResearchLet_Abramian.pdf file_size: 1117408 relation: main_file success: 1 file_date_updated: 2022-01-24T12:14:41Z has_accepted_license: '1' intvolume: ' 49' isi: 1 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: Geophysical Research Letters publication_identifier: eissn: - 1944-8007 issn: - 0094-8276 publication_status: published publisher: Wiley quality_controlled: '1' related_material: link: - relation: earlier_version url: https://doi.org/10.1002/essoar.10507697.1 scopus_import: '1' status: public title: Shear-convection interactions and orientation of 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: 4359f0d1-fa6c-11eb-b949-802e58b17ae8 volume: 49 year: '2022' ... --- _id: '12107' abstract: - lang: eng text: The sensitivity of coarse-grained daily extreme precipitation to sea surface temperature is analyzed using satellite precipitation estimates over the 300–302.5 K range. A theoretical scaling is proposed, linking changes in coarse-grained precipitation to changes in fine-scale hourly precipitation area fraction and changes in conditional fine-scale precipitation rates. The analysis reveals that the extreme coarse-grained precipitation scaling with temperature (∼7%/K) is dominated by the fine-scale precipitating fraction scaling (∼6.5%/K) when using a 3 mm/h fine-scale threshold to delineate the precipitating fraction. These results are shown to be robust to the selection of the precipitation product and to the percentile used to characterize the extreme. This new coarse-grained scaling is further related to the well-known scaling for fine-scale precipitation extremes, and suggests a compensation between thermodynamic and dynamic contributions or that both contributions are small with respect to that of fractional coverage. These results suggest that processes responsible for the changes in fractional coverage are to be accounted for to assess the sensitivity of coarse-grained extreme daily precipitation to surface temperature. acknowledgement: "We thank S. Cloché for her support with the handling of these various data sets. This study benefited from the IPSL mesocenter ESPRI facility which is supported by CNRS, UPMC, Labex L-IPSL, CNES and Ecole Polytechnique. We thank Rômulo A. Jucá Oliveira and Thomas\r\nFiolleau for helpful discussions on satellite data and precipitation. The authors acknowledge the CNES and CNRS support under the Megha-Tropiques program. C.M. gratefully acknowledges\r\nfunding from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation programme (Project CLUSTER, Grant agreement 805041). We further\r\nthank the reviewers for their insightful comments that improved the paper." article_number: e2022GL100624 article_processing_charge: No article_type: letter_note author: - first_name: Rémy full_name: Roca, Rémy last_name: Roca - first_name: Victorien full_name: De Meyer, Victorien last_name: De Meyer - 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: Roca R, De Meyer V, Muller CJ. Precipitating fraction, not intensity, explains extreme coarse-grained precipitation Clausius-Clapeyron scaling with sea surface temperature over tropical oceans. Geophysical Research Letters. 2022;49(24). doi:10.1029/2022GL100624 apa: Roca, R., De Meyer, V., & Muller, C. J. (2022). Precipitating fraction, not intensity, explains extreme coarse-grained precipitation Clausius-Clapeyron scaling with sea surface temperature over tropical oceans. Geophysical Research Letters. Wiley. https://doi.org/10.1029/2022GL100624 chicago: Roca, Rémy, Victorien De Meyer, and Caroline J Muller. “Precipitating Fraction, Not Intensity, Explains Extreme Coarse-Grained Precipitation Clausius-Clapeyron Scaling with Sea Surface Temperature over Tropical Oceans.” Geophysical Research Letters. Wiley, 2022. https://doi.org/10.1029/2022GL100624. ieee: R. Roca, V. De Meyer, and C. J. Muller, “Precipitating fraction, not intensity, explains extreme coarse-grained precipitation Clausius-Clapeyron scaling with sea surface temperature over tropical oceans,” Geophysical Research Letters, vol. 49, no. 24. Wiley, 2022. ista: Roca R, De Meyer V, Muller CJ. 2022. Precipitating fraction, not intensity, explains extreme coarse-grained precipitation Clausius-Clapeyron scaling with sea surface temperature over tropical oceans. Geophysical Research Letters. 49(24), e2022GL100624. mla: Roca, Rémy, et al. “Precipitating Fraction, Not Intensity, Explains Extreme Coarse-Grained Precipitation Clausius-Clapeyron Scaling with Sea Surface Temperature over Tropical Oceans.” Geophysical Research Letters, vol. 49, no. 24, e2022GL100624, Wiley, 2022, doi:10.1029/2022GL100624. short: R. Roca, V. De Meyer, C.J. Muller, Geophysical Research Letters 49 (2022). date_created: 2023-01-08T23:00:53Z date_published: 2022-12-28T00:00:00Z date_updated: 2023-08-03T14:10:27Z day: '28' ddc: - '550' department: - _id: CaMu doi: 10.1029/2022GL100624 external_id: isi: - '000924587900001' file: - access_level: open_access checksum: 2c6325cea8938adeea7e3a6f5c2ab64e content_type: application/pdf creator: dernst date_created: 2023-01-20T10:52:31Z date_updated: 2023-01-20T10:52:31Z file_id: '12326' file_name: 2022_GeophysicalResearchLetters_Roca.pdf file_size: 875379 relation: main_file success: 1 file_date_updated: 2023-01-20T10:52:31Z has_accepted_license: '1' intvolume: ' 49' isi: 1 issue: '24' language: - iso: eng month: '12' oa: 1 oa_version: Published Version 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: Precipitating fraction, not intensity, explains extreme coarse-grained precipitation Clausius-Clapeyron scaling with sea surface temperature over tropical oceans 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: 4359f0d1-fa6c-11eb-b949-802e58b17ae8 volume: 49 year: '2022' ... --- _id: '10656' abstract: - lang: eng text: Idealized simulations of the tropical atmosphere have predicted that clouds can spontaneously clump together in space, despite perfectly homogeneous settings. This phenomenon has been called self-aggregation, and it results in a state where a moist cloudy region with intense deep convective storms is surrounded by extremely dry subsiding air devoid of deep clouds. We review here the main findings from theoretical work and idealized models of this phenomenon, highlighting the physical processes believed to play a key role in convective self-aggregation. We also review the growing literature on the importance and implications of this phenomenon for the tropical atmosphere, notably, for the hydrological cycle and for precipitation extremes, in our current and in a warming climate. acknowledgement: 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 805041). She also thanks Grand Équipement National de Calcul Intensif (GENCI), France, for providing access to their computing platforms at Très Grand Centre de Calcul (TGCC). J.O.H. gratefully acknowledges funding from the Villum Foundation (grant 13168), the ERC under the Horizon 2020 research and innovation program (grant 771859), and the Novo Nordisk Foundation's Interdisciplinary Synergy Program (grant NNF19OC0057374). G.C. gratefully acknowledges the support of the transregional collaborative research center (SFB/TRR 165) “Waves to Weather” (http://www.wavestoweather.de) funded by the German Research Foundation (DFG). D.Y. is supported by a Packard Fellowship in Science and Engineering, the France–Berkeley Fund, Laboratory Directed Research and Development (LDRD) funding from the Lawrence Berkeley National Laboratory, and the US Department of Energy, Office of Science, Office of Biological and Environmental Research, Climate and Environmental Sciences Division, Regional and Global Climate Modeling Program under award DE-AC02-05CH11231. article_processing_charge: No article_type: original author: - 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: Da full_name: Yang, Da last_name: Yang - first_name: George full_name: Craig, George last_name: Craig - first_name: Timothy full_name: Cronin, Timothy last_name: Cronin - first_name: Benjamin full_name: Fildier, Benjamin last_name: Fildier - first_name: Jan O. full_name: Haerter, Jan O. last_name: Haerter - first_name: Cathy full_name: Hohenegger, Cathy last_name: Hohenegger - first_name: Brian full_name: Mapes, Brian last_name: Mapes - first_name: David full_name: Randall, David last_name: Randall - first_name: Sara full_name: Shamekh, Sara last_name: Shamekh - first_name: Steven C. full_name: Sherwood, Steven C. last_name: Sherwood citation: ama: Muller CJ, Yang D, Craig G, et al. Spontaneous aggregation of convective storms. Annual Review of Fluid Mechanics. 2022;54:133-157. doi:10.1146/annurev-fluid-022421-011319 apa: Muller, C. J., Yang, D., Craig, G., Cronin, T., Fildier, B., Haerter, J. O., … Sherwood, S. C. (2022). Spontaneous aggregation of convective storms. Annual Review of Fluid Mechanics. Annual Reviews. https://doi.org/10.1146/annurev-fluid-022421-011319 chicago: Muller, Caroline J, Da Yang, George Craig, Timothy Cronin, Benjamin Fildier, Jan O. Haerter, Cathy Hohenegger, et al. “Spontaneous Aggregation of Convective Storms.” Annual Review of Fluid Mechanics. Annual Reviews, 2022. https://doi.org/10.1146/annurev-fluid-022421-011319. ieee: C. J. Muller et al., “Spontaneous aggregation of convective storms,” Annual Review of Fluid Mechanics, vol. 54. Annual Reviews, pp. 133–157, 2022. ista: Muller CJ, Yang D, Craig G, Cronin T, Fildier B, Haerter JO, Hohenegger C, Mapes B, Randall D, Shamekh S, Sherwood SC. 2022. Spontaneous aggregation of convective storms. Annual Review of Fluid Mechanics. 54, 133–157. mla: Muller, Caroline J., et al. “Spontaneous Aggregation of Convective Storms.” Annual Review of Fluid Mechanics, vol. 54, Annual Reviews, 2022, pp. 133–57, doi:10.1146/annurev-fluid-022421-011319. short: C.J. Muller, D. Yang, G. Craig, T. Cronin, B. Fildier, J.O. Haerter, C. Hohenegger, B. Mapes, D. Randall, S. Shamekh, S.C. Sherwood, Annual Review of Fluid Mechanics 54 (2022) 133–157. date_created: 2022-01-23T23:01:29Z date_published: 2022-01-01T00:00:00Z date_updated: 2023-10-03T10:51:07Z day: '01' department: - _id: CaMu doi: 10.1146/annurev-fluid-022421-011319 ec_funded: 1 external_id: isi: - '000794152800006' intvolume: ' 54' isi: 1 language: - iso: eng main_file_link: - open_access: '1' url: https://doi.org/10.1146/annurev-fluid-022421-011319 month: '01' oa: 1 oa_version: Published Version page: 133-157 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: Annual Review of Fluid Mechanics publication_identifier: eissn: - 1545-4479 issn: - 0066-4189 publication_status: published publisher: Annual Reviews quality_controlled: '1' scopus_import: '1' status: public title: Spontaneous aggregation of convective storms type: journal_article user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87 volume: 54 year: '2022' ...