---
_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
license: https://creativecommons.org/licenses/by/4.0/
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: '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: '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
license: https://creativecommons.org/licenses/by-nc-nd/4.0/
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: '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: '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:
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checksum: 8cb88c1bc80ccee328478a62064d98f7
content_type: application/pdf
creator: dernst
date_created: 2024-01-24T11:19:54Z
date_updated: 2024-01-24T11:19:54Z
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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
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type: conference_abstract
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: '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
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...
---
_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: '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'
...
---
_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: '9151'
abstract:
- lang: eng
text: "We investigate how mesoscale circulations associated with convective aggregation
can modulate the sensitivity of the hydrologic cycle to warming. We quantify changes
in the full distribution of rain across radiative‐convective equilibrium states
in a cloud‐resolving model. For a given SST, the shift in mean rainfall between
disorganized and organized states is associated with a shift in atmospheric radiative
cooling, and is roughly analogous to the effect of a 4K SST increase. With rising
temperatures, the increase in mean rain rate is insensitive to the presence of
organization, while extremes can intensify faster in the aggregated state, leading
to a faster amplification in the sporadic nature of rain. When convection aggregates,
heavy rain is enhanced by 20‐30% and nonlinear behaviors are observed as a function
of SST and strength of aggregation feedbacks. First, radiative‐ and surface‐flux
aggregation feedbacks have multiplicative effects on extremes, illustrating a
non‐trivial sensitivity to the degree of organization. Second, alternating Clausius‐Clapeyron
and super‐Clausius‐Clapeyron regimes in extreme rainfall are found as a function
of SST, corresponding to varying thermodynamic and dynamic contributions, and
a large sensitivity to precipitation efficiency variations in some SST ranges.\r\nThe
potential for mesoscale circulations in amplifying the hydrologic cycle is established.
However these nonlinear distortions question the quantitative relevance of idealized
self‐aggregation. This calls for a deeper investigation of relationships which
capture the coupling between global energetics, aggregation feedbacks and local
convection, and for systematic tests of their sensitivity to domain configurations,
surface boundary conditions, microphysics and turbulence schemes."
article_number: e2020MS002256
article_processing_charge: No
article_type: original
author:
- first_name: Benjamin
full_name: Fildier, Benjamin
last_name: Fildier
- first_name: William D.
full_name: Collins, William D.
last_name: Collins
- 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: Fildier B, Collins WD, Muller CJ. Distortions of the rain distribution with
warming, with and without self‐aggregation. Journal of Advances in Modeling
Earth Systems. 2021;13(2). doi:10.1029/2020ms002256
apa: Fildier, B., Collins, W. D., & Muller, C. J. (2021). Distortions of the
rain distribution with warming, with and without self‐aggregation. Journal
of Advances in Modeling Earth Systems. American Geophysical Union. https://doi.org/10.1029/2020ms002256
chicago: Fildier, Benjamin, William D. Collins, and Caroline J Muller. “Distortions
of the Rain Distribution with Warming, with and without Self‐aggregation.” Journal
of Advances in Modeling Earth Systems. American Geophysical Union, 2021. https://doi.org/10.1029/2020ms002256.
ieee: B. Fildier, W. D. Collins, and C. J. Muller, “Distortions of the rain distribution
with warming, with and without self‐aggregation,” Journal of Advances in Modeling
Earth Systems, vol. 13, no. 2. American Geophysical Union, 2021.
ista: Fildier B, Collins WD, Muller CJ. 2021. Distortions of the rain distribution
with warming, with and without self‐aggregation. Journal of Advances in Modeling
Earth Systems. 13(2), e2020MS002256.
mla: Fildier, Benjamin, et al. “Distortions of the Rain Distribution with Warming,
with and without Self‐aggregation.” Journal of Advances in Modeling Earth Systems,
vol. 13, no. 2, e2020MS002256, American Geophysical Union, 2021, doi:10.1029/2020ms002256.
short: B. Fildier, W.D. Collins, C.J. Muller, Journal of Advances in Modeling Earth
Systems 13 (2021).
date_created: 2021-02-15T15:10:01Z
date_published: 2021-02-01T00:00:00Z
date_updated: 2022-01-24T12:26:01Z
day: '01'
ddc:
- '550'
doi: 10.1029/2020ms002256
extern: '1'
file:
- access_level: open_access
checksum: 591ce69b7a36f24346d2061ac712f0f4
content_type: application/pdf
creator: kschuh
date_created: 2021-08-11T12:23:01Z
date_updated: 2021-08-11T12:23:01Z
file_id: '9881'
file_name: 2021_JAMES_Fildier.pdf
file_size: 1947936
relation: main_file
success: 1
file_date_updated: 2021-08-11T12:23:01Z
has_accepted_license: '1'
intvolume: ' 13'
issue: '2'
keyword:
- Global and Planetary Change
- General Earth and Planetary Sciences
- Environmental Chemistry
language:
- iso: eng
license: https://creativecommons.org/licenses/by-nc/4.0/
month: '02'
oa: 1
oa_version: Published Version
publication: Journal of Advances in Modeling Earth Systems
publication_identifier:
issn:
- 1942-2466
- 1942-2466
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
scopus_import: '1'
status: public
title: Distortions of the rain distribution with warming, with and without self‐aggregation
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: 8b945eb4-e2f2-11eb-945a-df72226e66a9
volume: 13
year: '2021'
...
---
_id: '9124'
abstract:
- lang: eng
text: The couplings among clouds, convection, and circulation in trade-wind regimes
remain a fundamental puzzle that limits our ability to constrain future climate
change. Radiative heating plays an important role in these couplings. Here we
calculate the clear-sky radiative profiles from 2001 in-situ soundings (978 dropsondes
and 1023 radiosondes) collected during the EUREC4A field campaign, which took
place south and east of Barbados in January–February 2020. We describe the method
used to calculate these radiative profiles and present preliminary results sampling
variability at multiple scales, from the variability across all soundings to groupings
by diurnal cycle and mesoscale organization state, as well as individual soundings
associated with elevated moisture layers. This clear-sky radiative profiles data
set can provide important missing detail to what can be learned from calculations
based on passive remote sensing and help in investigating the role of radiation
in dynamic and thermodynamic variability in trade-wind regimes. All data are archived
and freely available for public access on AERIS (Albright et al. (2020), https://doi.org/10.25326/78).
article_processing_charge: No
author:
- first_name: Anna Lea
full_name: Albright, Anna Lea
last_name: Albright
- first_name: Benjamin
full_name: Fildier, Benjamin
last_name: Fildier
- first_name: Ludovic
full_name: Touzé-Peiffer, Ludovic
last_name: Touzé-Peiffer
- first_name: Robert
full_name: Pincus, Robert
last_name: Pincus
- first_name: Jessica
full_name: Vial, Jessica
last_name: Vial
- 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: Albright AL, Fildier B, Touzé-Peiffer L, Pincus R, Vial J, Muller CJ. Atmospheric
radiative profiles during EUREC4A. Earth System Science Data. doi:10.5194/essd-2020-269
apa: Albright, A. L., Fildier, B., Touzé-Peiffer, L., Pincus, R., Vial, J., &
Muller, C. J. (n.d.). Atmospheric radiative profiles during EUREC4A. Earth
System Science Data. Copernicus Publications. https://doi.org/10.5194/essd-2020-269
chicago: Albright, Anna Lea, Benjamin Fildier, Ludovic Touzé-Peiffer, Robert Pincus,
Jessica Vial, and Caroline J Muller. “Atmospheric Radiative Profiles during EUREC4A.”
Earth System Science Data. Copernicus Publications, n.d. https://doi.org/10.5194/essd-2020-269.
ieee: A. L. Albright, B. Fildier, L. Touzé-Peiffer, R. Pincus, J. Vial, and C. J.
Muller, “Atmospheric radiative profiles during EUREC4A,” Earth System Science
Data. Copernicus Publications.
ista: Albright AL, Fildier B, Touzé-Peiffer L, Pincus R, Vial J, Muller CJ. Atmospheric
radiative profiles during EUREC4A. Earth System Science Data, 10.5194/essd-2020-269.
mla: Albright, Anna Lea, et al. “Atmospheric Radiative Profiles during EUREC4A.”
Earth System Science Data, Copernicus Publications, doi:10.5194/essd-2020-269.
short: A.L. Albright, B. Fildier, L. Touzé-Peiffer, R. Pincus, J. Vial, C.J. Muller,
Earth System Science Data (n.d.).
date_created: 2021-02-15T14:05:54Z
date_published: 2020-09-24T00:00:00Z
date_updated: 2022-01-24T12:27:08Z
day: '24'
doi: 10.5194/essd-2020-269
extern: '1'
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.5194/essd-2020-269
month: '09'
oa: 1
oa_version: Preprint
publication: Earth System Science Data
publication_status: submitted
publisher: Copernicus Publications
status: public
title: Atmospheric radiative profiles during EUREC4A
type: preprint
user_id: 8b945eb4-e2f2-11eb-945a-df72226e66a9
year: '2020'
...
---
_id: '9125'
abstract:
- lang: eng
text: This study investigates the feedbacks between an interactive sea surface temperature
(SST) and the self‐aggregation of deep convective clouds, using a cloud‐resolving
model in nonrotating radiative‐convective equilibrium. The ocean is modeled as
one layer slab with a temporally fixed mean but spatially varying temperature.
We find that the interactive SST decelerates the aggregation and that the deceleration
is larger with a shallower slab, consistent with earlier studies. The surface
temperature anomaly in dry regions is positive at first, thus opposing the diverging
shallow circulation known to favor self‐aggregation, consistent with the slower
aggregation. But surprisingly, the driest columns then have a negative SST anomaly,
thus strengthening the diverging shallow circulation and favoring aggregation.
This diverging circulation out of dry regions is found to be well correlated with
the aggregation speed. It can be linked to a positive surface pressure anomaly
(PSFC), itself the consequence of SST anomalies and boundary layer radiative cooling.
The latter cools and dries the boundary layer, thus increasing PSFC anomalies
through virtual effects and hydrostasy. Sensitivity experiments confirm the key
role played by boundary layer radiative cooling in determining PSFC anomalies
in dry regions, and thus the shallow diverging circulation and the aggregation
speed.
article_number: e2020MS002164
article_processing_charge: No
article_type: original
author:
- first_name: S.
full_name: Shamekh, S.
last_name: Shamekh
- 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: J.‐P.
full_name: Duvel, J.‐P.
last_name: Duvel
- first_name: F.
full_name: D'Andrea, F.
last_name: D'Andrea
citation:
ama: Shamekh S, Muller CJ, Duvel J ‐P., D’Andrea F. Self‐aggregation of convective
clouds with interactive sea surface temperature. Journal of Advances in Modeling
Earth Systems. 2020;12(11). doi:10.1029/2020ms002164
apa: Shamekh, S., Muller, C. J., Duvel, J. ‐P., & D’Andrea, F. (2020). Self‐aggregation
of convective clouds with interactive sea surface temperature. Journal of Advances
in Modeling Earth Systems. American Geophysical Union. https://doi.org/10.1029/2020ms002164
chicago: Shamekh, S., Caroline J Muller, J.‐P. Duvel, and F. D’Andrea. “Self‐aggregation
of Convective Clouds with Interactive Sea Surface Temperature.” Journal of
Advances in Modeling Earth Systems. American Geophysical Union, 2020. https://doi.org/10.1029/2020ms002164.
ieee: S. Shamekh, C. J. Muller, J. ‐P. Duvel, and F. D’Andrea, “Self‐aggregation
of convective clouds with interactive sea surface temperature,” Journal of
Advances in Modeling Earth Systems, vol. 12, no. 11. American Geophysical
Union, 2020.
ista: Shamekh S, Muller CJ, Duvel J ‐P., D’Andrea F. 2020. Self‐aggregation of convective
clouds with interactive sea surface temperature. Journal of Advances in Modeling
Earth Systems. 12(11), e2020MS002164.
mla: Shamekh, S., et al. “Self‐aggregation of Convective Clouds with Interactive
Sea Surface Temperature.” Journal of Advances in Modeling Earth Systems,
vol. 12, no. 11, e2020MS002164, American Geophysical Union, 2020, doi:10.1029/2020ms002164.
short: S. Shamekh, C.J. Muller, J. ‐P. Duvel, F. D’Andrea, Journal of Advances in
Modeling Earth Systems 12 (2020).
date_created: 2021-02-15T14:06:23Z
date_published: 2020-11-01T00:00:00Z
date_updated: 2022-01-24T12:27:38Z
day: '01'
doi: 10.1029/2020ms002164
extern: '1'
intvolume: ' 12'
issue: '11'
keyword:
- Global and Planetary Change
- General Earth and Planetary Sciences
- Environmental Chemistry
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1029/2020MS002164
month: '11'
oa: 1
oa_version: Published Version
publication: Journal of Advances in Modeling Earth Systems
publication_identifier:
issn:
- 1942-2466
- 1942-2466
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
status: public
title: Self‐aggregation of convective clouds with interactive sea surface temperature
type: journal_article
user_id: 8b945eb4-e2f2-11eb-945a-df72226e66a9
volume: 12
year: '2020'
...
---
_id: '9126'
abstract:
- lang: eng
text: The goal of this study is to understand the mechanisms controlling the isotopic
composition of the water vapor near the surface of tropical oceans, at the scale
of about a hundred kilometers and a month. In the tropics, it has long been observed
that the isotopic compositions of rain and vapor near the surface are more depleted
when the precipitation rate is high. This is called the “amount effect.” Previous
studies, based on observations or models with parameterized convection, have highlighted
the roles of deep convective and mesoscale downdrafts and rain evaporation. But
the relative importance of these processes has never been quantified. We hypothesize
that it can be quantified using an analytical model constrained by large‐eddy
simulations. Results from large‐eddy simulations confirm that the classical amount
effect can be simulated only if precipitation rate changes result from changes
in the large‐scale circulation. We find that the main process depleting the water
vapor compared to the equilibrium with the ocean is the fact that updrafts stem
from areas where the water vapor is more enriched. The main process responsible
for the amount effect is the fact that when the large‐scale ascent increases,
isotopic vertical gradients are steeper, so that updrafts and downdrafts deplete
the subcloud layer more efficiently.
article_number: e2020MS002106
article_processing_charge: No
article_type: original
author:
- first_name: Camille
full_name: Risi, Camille
last_name: Risi
- 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: Peter
full_name: Blossey, Peter
last_name: Blossey
citation:
ama: Risi C, Muller CJ, Blossey P. What controls the water vapor isotopic composition
near the surface of tropical oceans? Results from an analytical model constrained
by large‐eddy simulations. Journal of Advances in Modeling Earth Systems.
2020;12(8). doi:10.1029/2020ms002106
apa: Risi, C., Muller, C. J., & Blossey, P. (2020). What controls the water
vapor isotopic composition near the surface of tropical oceans? Results from an
analytical model constrained by large‐eddy simulations. Journal of Advances
in Modeling Earth Systems. American Geophysical Union. https://doi.org/10.1029/2020ms002106
chicago: Risi, Camille, Caroline J Muller, and Peter Blossey. “What Controls the
Water Vapor Isotopic Composition near the Surface of Tropical Oceans? Results
from an Analytical Model Constrained by Large‐eddy Simulations.” Journal of
Advances in Modeling Earth Systems. American Geophysical Union, 2020. https://doi.org/10.1029/2020ms002106.
ieee: C. Risi, C. J. Muller, and P. Blossey, “What controls the water vapor isotopic
composition near the surface of tropical oceans? Results from an analytical model
constrained by large‐eddy simulations,” Journal of Advances in Modeling Earth
Systems, vol. 12, no. 8. American Geophysical Union, 2020.
ista: Risi C, Muller CJ, Blossey P. 2020. What controls the water vapor isotopic
composition near the surface of tropical oceans? Results from an analytical model
constrained by large‐eddy simulations. Journal of Advances in Modeling Earth Systems.
12(8), e2020MS002106.
mla: Risi, Camille, et al. “What Controls the Water Vapor Isotopic Composition near
the Surface of Tropical Oceans? Results from an Analytical Model Constrained by
Large‐eddy Simulations.” Journal of Advances in Modeling Earth Systems,
vol. 12, no. 8, e2020MS002106, American Geophysical Union, 2020, doi:10.1029/2020ms002106.
short: C. Risi, C.J. Muller, P. Blossey, Journal of Advances in Modeling Earth Systems
12 (2020).
date_created: 2021-02-15T14:06:38Z
date_published: 2020-08-01T00:00:00Z
date_updated: 2022-01-24T12:28:12Z
day: '01'
doi: 10.1029/2020ms002106
extern: '1'
intvolume: ' 12'
issue: '8'
keyword:
- Global and Planetary Change
- General Earth and Planetary Sciences
- Environmental Chemistry
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1029/2020MS002106
month: '08'
oa: 1
oa_version: Published Version
publication: Journal of Advances in Modeling Earth Systems
publication_identifier:
issn:
- 1942-2466
- 1942-2466
publication_status: published
publisher: American Geophysical Union
quality_controlled: '1'
status: public
title: What controls the water vapor isotopic composition near the surface of tropical
oceans? Results from an analytical model constrained by large‐eddy simulations
type: journal_article
user_id: 8b945eb4-e2f2-11eb-945a-df72226e66a9
volume: 12
year: '2020'
...
---
_id: '9127'
abstract:
- lang: eng
text: Nearly all regions in the world are projected to become dryer in a warming
climate. Here, we investigate the Mediterranean region, often referred to as a
climate change “hot spot”. From regional climate simulations, it is shown that
although enhanced warming and drying over land is projected, the spatial pattern
displays high variability. Indeed, drying is largely caused by enhanced warming
over land. However, in Northern Europe, soil moisture alleviates warming induced
drying by up to 50% due to humidity uptake from land. In already arid regions,
the Mediterranean Sea is generally the only humidity source, and drying is only
due to land warming. However, over Sahara and the Iberian Peninsula, enhanced
warming over land is insufficient to explain the extreme drying. These regions
are also isolated from humidity advection by heat lows, which are cyclonic circulation
anomalies associated with surface heating over land. The cyclonic circulation
scales with the temperature gradient between land and ocean which increases with
climate change, reinforcing the cyclonic circulation over Sahara and the Iberian
Peninsula, both diverting the zonal advection of humidity to the south of the
Iberian Peninsula. The dynamics are therefore key in the warming and drying of
the Mediterranean region, with extreme aridification over the Sahara and Iberian
Peninsula. In these regions, the risk for human health due to the thermal load
which accounts for air temperature and humidity is therefore projected to increase
significantly with climate change at a level of extreme danger.
article_number: '78'
article_processing_charge: No
article_type: original
author:
- first_name: Philippe
full_name: Drobinski, Philippe
last_name: Drobinski
- first_name: Nicolas
full_name: Da Silva, Nicolas
last_name: Da Silva
- first_name: Sophie
full_name: Bastin, Sophie
last_name: Bastin
- first_name: Sylvain
full_name: Mailler, Sylvain
last_name: Mailler
- 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: Bodo
full_name: Ahrens, Bodo
last_name: Ahrens
- first_name: Ole B.
full_name: Christensen, Ole B.
last_name: Christensen
- first_name: Piero
full_name: Lionello, Piero
last_name: Lionello
citation:
ama: Drobinski P, Da Silva N, Bastin S, et al. How warmer and drier will the Mediterranean
region be at the end of the twenty-first century? Regional Environmental Change.
2020;20(9). doi:10.1007/s10113-020-01659-w
apa: Drobinski, P., Da Silva, N., Bastin, S., Mailler, S., Muller, C. J., Ahrens,
B., … Lionello, P. (2020). How warmer and drier will the Mediterranean region
be at the end of the twenty-first century? Regional Environmental Change.
Springer Nature. https://doi.org/10.1007/s10113-020-01659-w
chicago: Drobinski, Philippe, Nicolas Da Silva, Sophie Bastin, Sylvain Mailler,
Caroline J Muller, Bodo Ahrens, Ole B. Christensen, and Piero Lionello. “How Warmer
and Drier Will the Mediterranean Region Be at the End of the Twenty-First Century?”
Regional Environmental Change. Springer Nature, 2020. https://doi.org/10.1007/s10113-020-01659-w.
ieee: P. Drobinski et al., “How warmer and drier will the Mediterranean region
be at the end of the twenty-first century?,” Regional Environmental Change,
vol. 20, no. 9. Springer Nature, 2020.
ista: Drobinski P, Da Silva N, Bastin S, Mailler S, Muller CJ, Ahrens B, Christensen
OB, Lionello P. 2020. How warmer and drier will the Mediterranean region be at
the end of the twenty-first century? Regional Environmental Change. 20(9), 78.
mla: Drobinski, Philippe, et al. “How Warmer and Drier Will the Mediterranean Region
Be at the End of the Twenty-First Century?” Regional Environmental Change,
vol. 20, no. 9, 78, Springer Nature, 2020, doi:10.1007/s10113-020-01659-w.
short: P. Drobinski, N. Da Silva, S. Bastin, S. Mailler, C.J. Muller, B. Ahrens,
O.B. Christensen, P. Lionello, Regional Environmental Change 20 (2020).
date_created: 2021-02-15T14:06:58Z
date_published: 2020-09-11T00:00:00Z
date_updated: 2022-01-24T12:28:49Z
day: '11'
doi: 10.1007/s10113-020-01659-w
extern: '1'
intvolume: ' 20'
issue: '9'
keyword:
- Global and Planetary Change
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://hal-insu.archives-ouvertes.fr/insu-02881534
month: '09'
oa: 1
oa_version: Submitted Version
publication: Regional Environmental Change
publication_identifier:
issn:
- 1436-3798
- 1436-378X
publication_status: published
publisher: Springer Nature
quality_controlled: '1'
status: public
title: How warmer and drier will the Mediterranean region be at the end of the twenty-first
century?
type: journal_article
user_id: 8b945eb4-e2f2-11eb-945a-df72226e66a9
volume: 20
year: '2020'
...
---
_id: '9128'
abstract:
- lang: eng
text: This paper reviews recent important advances in our understanding of the response
of precipitation extremes to warming from theory and from idealized cloud-resolving
simulations. A theoretical scaling for precipitation extremes has been proposed
and refined in the past decades, allowing to address separately the contributions
from the thermodynamics, the dynamics and the microphysics. Theoretical constraints,
as well as remaining uncertainties, associated with each of these three contributions
to precipitation extremes, are discussed. Notably, although to leading order precipitation
extremes seem to follow the thermodynamic theoretical expectation in idealized
simulations, considerable uncertainty remains regarding the response of the dynamics
and of the microphysics to warming, and considerable departure from this theoretical
expectation is found in observations and in more realistic simulations. We also
emphasize key outstanding questions, in particular the response of mesoscale convective
organization to warming. Observations suggest that extreme rainfall often comes
from an organized system in very moist environments. Improved understanding of
the physical processes behind convective organization is needed in order to achieve
accurate extreme rainfall prediction in our current, and in a warming climate.
article_number: '035001'
article_processing_charge: No
article_type: letter_note
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: Yukari
full_name: Takayabu, Yukari
last_name: Takayabu
citation:
ama: 'Muller CJ, Takayabu Y. Response of precipitation extremes to warming: What
have we learned from theory and idealized cloud-resolving simulations, and what
remains to be learned? Environmental Research Letters. 2020;15(3). doi:10.1088/1748-9326/ab7130'
apa: 'Muller, C. J., & Takayabu, Y. (2020). Response of precipitation extremes
to warming: What have we learned from theory and idealized cloud-resolving simulations,
and what remains to be learned? Environmental Research Letters. IOP Publishing.
https://doi.org/10.1088/1748-9326/ab7130'
chicago: 'Muller, Caroline J, and Yukari Takayabu. “Response of Precipitation Extremes
to Warming: What Have We Learned from Theory and Idealized Cloud-Resolving Simulations,
and What Remains to Be Learned?” Environmental Research Letters. IOP Publishing,
2020. https://doi.org/10.1088/1748-9326/ab7130.'
ieee: 'C. J. Muller and Y. Takayabu, “Response of precipitation extremes to warming:
What have we learned from theory and idealized cloud-resolving simulations, and
what remains to be learned?,” Environmental Research Letters, vol. 15,
no. 3. IOP Publishing, 2020.'
ista: 'Muller CJ, Takayabu Y. 2020. Response of precipitation extremes to warming:
What have we learned from theory and idealized cloud-resolving simulations, and
what remains to be learned? Environmental Research Letters. 15(3), 035001.'
mla: 'Muller, Caroline J., and Yukari Takayabu. “Response of Precipitation Extremes
to Warming: What Have We Learned from Theory and Idealized Cloud-Resolving Simulations,
and What Remains to Be Learned?” Environmental Research Letters, vol. 15,
no. 3, 035001, IOP Publishing, 2020, doi:10.1088/1748-9326/ab7130.'
short: C.J. Muller, Y. Takayabu, Environmental Research Letters 15 (2020).
date_created: 2021-02-15T14:07:14Z
date_published: 2020-02-18T00:00:00Z
date_updated: 2022-01-24T12:29:46Z
day: '18'
doi: 10.1088/1748-9326/ab7130
extern: '1'
intvolume: ' 15'
issue: '3'
keyword:
- Renewable Energy
- Sustainability and the Environment
- Public Health
- Environmental and Occupational Health
- General Environmental Science
language:
- iso: eng
main_file_link:
- open_access: '1'
url: https://doi.org/10.1088/1748-9326/ab7130
month: '02'
oa: 1
oa_version: Published Version
publication: Environmental Research Letters
publication_identifier:
issn:
- 1748-9326
publication_status: published
publisher: IOP Publishing
quality_controlled: '1'
status: public
title: 'Response of precipitation extremes to warming: What have we learned from theory
and idealized cloud-resolving simulations, and what remains to be learned?'
type: journal_article
user_id: 8b945eb4-e2f2-11eb-945a-df72226e66a9
volume: 15
year: '2020'
...