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Title: A Refined Understanding of the Ice Cloud Longwave Scattering Effects in Climate Model

Journal Article · · Journal of Advances in Modeling Earth Systems
DOI:https://doi.org/10.1029/2023MS003810· OSTI ID:2007440
ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [1];  [3]; ORCiD logo [4]; ORCiD logo [1]
  1. Department of Climate and Space Sciences and Engineering the University of Michigan Ann Arbor MI USA
  2. Department of Climate and Space Sciences and Engineering the University of Michigan Ann Arbor MI USA, Now at Research Center for Environmental Changes Academia Sinica Taipei Taiwan
  3. Environmental &, Climate Sciences Department Brookhaven National Laboratory New York State NY USA
  4. Department of Atmospheric Sciences Texas A&,M University College Station TX USA

Abstract Because longwave (LW) absorption by greenhouse gases and clouds is more significant than the LW scattering effect by clouds, most climate models neglect cloud LW scattering to save computational costs. Ignoring cloud LW scattering directly overestimates outgoing longwave radiation (OLR). This study included ice‐cloud LW scattering treatment in the Exascale Energy Earth System Model (E3SM) version 2 and ran fully‐coupled simulations, prescribed sea surface temperature simulations, and offline radiative transfer calculations to comprehensively assess the impact of ice‐cloud LW scattering on global climate simulation. The instantaneous effect due to ice‐cloud LW scattering reduces the OLR by ∼1 W/m 2 on the global average and 2 W/m 2 on the tropical average. Tropospheric warming and high cloud amount reduction act to partially compensate for such instantaneous OLR reduction caused by the inclusion of LW scattering. When the simulation reaches the equilibrium, the surface warms by 0.66 K on average with respect to the simulation without LW scattering, with the Arctic surface temperature differences more than twice as large as that of the global mean. The impact of including LW scattering on the simulated climate change in response to 4 × CO 2 is also assessed. While including the cloud LW scattering does not significantly modify radiative forcing and total radiative feedback under such a scenario, it results in a 10% more positive cloud feedback.

Research Organization:
Brookhaven National Laboratory (BNL), Upton, NY (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER); National Aeronautics and Space Administration (NASA)
Grant/Contract Number:
DE‐SC0019278; DE‐SC0022117; SC0012704; SC0019278; SC0022117; 80NSSC22K1433
OSTI ID:
2007440
Alternate ID(s):
OSTI ID: 2203788; OSTI ID: 2204129
Report Number(s):
BNL-224915-2023-JAAM; e2023MS003810
Journal Information:
Journal of Advances in Modeling Earth Systems, Journal Name: Journal of Advances in Modeling Earth Systems Vol. 15 Journal Issue: 10; ISSN 1942-2466
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

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