Dissecting Anvil Cloud Response to Sea Surface Warming

Dissecting Anvil Cloud Response to Sea Surface Warming
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剖析砧云对海面变暖的反应

DOI:
10.1029/2021gl094049
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发表时间:
2021
影响因子:
5.2
通讯作者:
A. S. Donahue
A. S. Donahue
中科院分区:
地球科学1区
文献类型:
--
作者:
H. Beydoun;P. Caldwell;W. Hannah;A. S. Donahue

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We derive an anvil cloud diagnostic from the continuity equation of cloud ice and apply it to the output of convection‐permitting Energy Exascale Earth System Model (E3SM) simulations run in radiative‐convective equilibrium mode. This diagnostic shows that anvil cloud fraction can be reliably diagnosed as a product of cloud detrainment and lifetime. Detrainment is found to be approximated well by a product of clear sky convergence and cloud ice mixing ratio, while cloud lifetime is dominated by sedimentation. Taken together, this diagnostic expresses anvil cloud fraction as a function of five physically measurable quantities. Of these, clear‐sky convergence changes drive the anvil cloud reduction with warming while an increase in cloud ice mixing ratio buffers the decrease. Accordingly, this study provides a theoretical foundation upon which the Stability‐Iris hypothesis can be tested.
DOI: 10.1029/2020ms002138
发表时间: 2020-09
影响因子: 6.8
作者:
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