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Title: Sources of Intermodel Spread in the Lapse Rate and Water Vapor Feedbacks

Journal Article · · Journal of Climate
 [1];  [2];  [3];  [1];  [1];  [3]
  1. Lawrence Livermore National Laboratory, Livermore, California
  2. Department of Atmospheric Sciences, and School of Oceanography, University of Washington, Seattle, Washington
  3. Department of Atmospheric Sciences, University of Washington, Seattle, Washington

Abstract Sources of intermodel differences in the global lapse rate (LR) and water vapor (WV) feedbacks are assessed using CO2 forcing simulations from 28 general circulation models. Tropical surface warming leads to significant warming and moistening in the tropical and extratropical upper troposphere, signifying a nonlocal, tropical influence on extratropical radiation and feedbacks. Model spread in the locally defined LR and WV feedbacks is pronounced in the Southern Ocean because of large-scale ocean upwelling, which reduces surface warming and decouples the surface from the tropospheric response. The magnitude of local extratropical feedbacks across models and over time is well characterized using the ratio of tropical to extratropical surface warming. It is shown that model differences in locally defined LR and WV feedbacks, particularly over the southern extratropics, drive model variability in the global feedbacks. The cross-model correlation between the global LR and WV feedbacks therefore does not arise from their covariation in the tropics, but rather from the pattern of warming exerting a common control on extratropical feedback responses. Because local feedbacks over the Southern Hemisphere are an important contributor to the global feedback, the partitioning of surface warming between the tropics and the southern extratropics is a key determinant of the spread in the global LR and WV feedbacks. It is also shown that model Antarctic sea ice climatology influences sea ice area changes and southern extratropical surface warming. As a result, model discrepancies in climatological Antarctic sea ice area have a significant impact on the intermodel spread of the global LR and WV feedbacks.

Research Organization:
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE; National Science Foundation (NSF); National Aeronautics and Space Administration (NASA)
Grant/Contract Number:
AC52-07NA27344; NNX13AN49G
OSTI ID:
1633937
Alternate ID(s):
OSTI ID: 1438795
Report Number(s):
LLNL-JRNL-739332
Journal Information:
Journal of Climate, Journal Name: Journal of Climate Vol. 31 Journal Issue: 8; ISSN 0894-8755
Publisher:
American Meteorological SocietyCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 28 works
Citation information provided by
Web of Science

Cited By (4)

ESD Reviews: Climate feedbacks in the Earth system and prospects for their evaluation journal January 2019
Sources of Uncertainty in the Meridional Pattern of Climate Change journal September 2018
Explaining Differences Between Recent Model and Satellite Tropospheric Warming Rates With Tropical SSTs journal August 2019
Climatology Explains Intermodel Spread in Tropical Upper Tropospheric Cloud and Relative Humidity Response to Greenhouse Warming journal November 2019

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