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Title: Thermodynamic control of anvil cloud amount

Abstract

General circulation models show that as the surface temperature increases, the convective anvil clouds shrink. By analyzing radiative–convective equilibrium simulations, our work shows that this behavior is rooted in basic energetic and thermodynamic properties of the atmosphere: As the climate warms, the clouds rise and remain at nearly the same temperature, but find themselves in a more stable atmosphere; this enhanced stability reduces the convective outflow in the upper troposphere and decreases the anvil cloud fraction. By warming the troposphere and increasing the upper-tropospheric stability, the clustering of deep convection also reduces the convective outflow and the anvil cloud fraction. When clouds are radiatively active, this robust coupling between temperature, high clouds, and circulation exerts a positive feedback on convective aggregation and favors the maintenance of strongly aggregated atmospheric states at high temperatures. This stability iris mechanism likely contributes to the narrowing of rainy areas as the climate warms. Whether or not it influences climate sensitivity requires further investigation.

Authors:
 [1];  [2];  [1];  [2];  [3];  [4]; ORCiD logo [5]
  1. Paris-Sorbonne and Pierre-and-Marie Curie (UPMC) Univ., Paris (France). Dynamic Meteorology Lab. (LMD)/Inst. Pierre Simon Laplace (IPSL)
  2. Max-Planck Inst. for Meteorology, Hamburg (Germany)
  3. Stony Brook Univ., NY (United States). School of Marine and Atmospheric Sciences
  4. Columbia Univ., New York, NY (United States). Lamont–Doherty Earth Observatory
  5. National Center for Atmospheric Research, Boulder, CO (United States). Climate and Global Dynamics Lab.
Publication Date:
Research Org.:
Univ. Corp. for Atmospheric Research (UCAR), Boulder, Co (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23). Climate and Environmental Sciences Division; National Centre for Scientific Research (CNRS), Strasbourg (France); National Research Agency (ANR); Max-Planck Society; German Research Foundation (DFG)
OSTI Identifier:
1262439
Alternate Identifier(s):
OSTI ID: 1438340
Grant/Contract Number:  
FC02-97ER62402; ANR-10-LABX-0018; VO 1765/3-1
Resource Type:
Published Article
Journal Name:
Proceedings of the National Academy of Sciences of the United States of America
Additional Journal Information:
Journal Name: Proceedings of the National Academy of Sciences of the United States of America Journal Volume: 113 Journal Issue: 32; Journal ID: ISSN 0027-8424
Publisher:
National Academy of Sciences, Washington, DC (United States)
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; anvil cloud; cloud feedback; convective aggregation; large-scale circulation; climate sensitivity

Citation Formats

Bony, Sandrine, Stevens, Bjorn, Coppin, David, Becker, Tobias, Reed, Kevin A., Voigt, Aiko, and Medeiros, Brian. Thermodynamic control of anvil cloud amount. United States: N. p., 2016. Web. doi:10.1073/pnas.1601472113.
Bony, Sandrine, Stevens, Bjorn, Coppin, David, Becker, Tobias, Reed, Kevin A., Voigt, Aiko, & Medeiros, Brian. Thermodynamic control of anvil cloud amount. United States. doi:10.1073/pnas.1601472113.
Bony, Sandrine, Stevens, Bjorn, Coppin, David, Becker, Tobias, Reed, Kevin A., Voigt, Aiko, and Medeiros, Brian. Wed . "Thermodynamic control of anvil cloud amount". United States. doi:10.1073/pnas.1601472113.
@article{osti_1262439,
title = {Thermodynamic control of anvil cloud amount},
author = {Bony, Sandrine and Stevens, Bjorn and Coppin, David and Becker, Tobias and Reed, Kevin A. and Voigt, Aiko and Medeiros, Brian},
abstractNote = {General circulation models show that as the surface temperature increases, the convective anvil clouds shrink. By analyzing radiative–convective equilibrium simulations, our work shows that this behavior is rooted in basic energetic and thermodynamic properties of the atmosphere: As the climate warms, the clouds rise and remain at nearly the same temperature, but find themselves in a more stable atmosphere; this enhanced stability reduces the convective outflow in the upper troposphere and decreases the anvil cloud fraction. By warming the troposphere and increasing the upper-tropospheric stability, the clustering of deep convection also reduces the convective outflow and the anvil cloud fraction. When clouds are radiatively active, this robust coupling between temperature, high clouds, and circulation exerts a positive feedback on convective aggregation and favors the maintenance of strongly aggregated atmospheric states at high temperatures. This stability iris mechanism likely contributes to the narrowing of rainy areas as the climate warms. Whether or not it influences climate sensitivity requires further investigation.},
doi = {10.1073/pnas.1601472113},
journal = {Proceedings of the National Academy of Sciences of the United States of America},
number = 32,
volume = 113,
place = {United States},
year = {2016},
month = {7}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record
DOI: 10.1073/pnas.1601472113

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Cited by: 24 works
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