Why Is Climate Sensitivity for Solar Forcing Smaller than for an Equivalent CO2 Forcing?

被引:7
作者
Kaur, Harpreet [1 ]
Bala, Govindasamy [1 ]
Seshadri, Ashwin K. [1 ,2 ]
机构
[1] Indian Inst Sci, Ctr Atmospher & Ocean Sci, Bangalore, India
[2] Indian Inst Sci, Divecha Ctr Climate Change, Bangalore, India
关键词
Climate change; Climate sensitivity; Radiative fluxes; Radiative forcing; Climate models; General circulation models; SURFACE-TEMPERATURE-CHANGE; RADIATIVE KERNEL TECHNIQUE; LOW-CLOUD COVER; FEEDBACK PROCESSES; TROPOSPHERIC ADJUSTMENT; IRRADIANCE REDUCTION; EVOLVING PATTERNS; GLOBAL CLOUD; WATER-VAPOR; LAPSE-RATE;
D O I
10.1175/JCLI-D-21-0980.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Previous studies have shown that climate sensitivity, defined as the global mean surface temperature change per unit radiative forcing, is smaller for solar radiative forcing compared to an equivalent CO2 radiative forcing. We investigate the causes for this difference using the NCAR CAM4 model. The contributions to the climate feedback parameter, which is inversely related to climate sensitivity, are estimated for water vapor, lapse rate, Planck, albedo, and cloud feedbacks using the radiative kernel technique. The total feedback estimated for CO2 and solar radiative forcing from our model simulations is -1.23 and -1.45 W m(-2) K-1, respectively. We find that the difference in feedback between the two cases is primarily due to differences in lapse rate, water vapor, and cloud feedbacks, which together explain 65% of the difference in total feedback. The rest comes from Planck and albedo feedbacks. The differences in feedbacks arise mainly from differences in the horizontal (meridional) structure of forcing and the consequent warming. Our study provides important insights into the effects of the meridional structure of forcing on climate feedback, which is important for evaluating global climate change from different forcing agents. Significance StatementAn increase in atmospheric CO2 concentration or an increase in incoming solar radiation leads to a rise in the radiative budget and consequent climate warming, which is amplified by the presence of multiple climate feedbacks. These feedbacks, from changes in surface albedo, combined effect of water vapor and the vertical lapse rate of temperature, and changes in clouds, differ between solar and CO2 forcing. Using radiative kernels, this study quantifies these individual feedbacks for an equivalent radiative change caused by an increase in CO2 or incoming solar radiation, showing how the differences arise from differences in the meridional patterns of warming. In agreement with prior studies, these differences can explain the smaller efficacy of solar forcing compared to CO2 forcing.
引用
收藏
页码:775 / 789
页数:15
相关论文
共 50 条
[41]   Understanding the Rapid Precipitation Response to CO2 and Aerosol Forcing on a Regional Scale [J].
Richardson, Thomas B. ;
Forster, Piers M. ;
Andrews, Timothy ;
Parker, Doug J. .
JOURNAL OF CLIMATE, 2016, 29 (02) :583-594
[42]   On the response of the climate system to solar forcing - Introductory paper [J].
Bengtsson, L. .
SPACE SCIENCE REVIEWS, 2006, 125 (1-4) :187-197
[43]   Influences of Solar Forcing at Ultraviolet and Longer Wavelengths on Climate [J].
Shindell, Drew T. ;
Faluvegi, Greg ;
Schmidt, Gavin A. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2020, 125 (07)
[44]   Understanding nonlinear tropical precipitation responses to CO2 forcing [J].
Chadwick, Robin ;
Good, Peter .
GEOPHYSICAL RESEARCH LETTERS, 2013, 40 (18) :4911-4915
[45]   Role of sea surface temperature patterns for the Southern Hemisphere jet stream response to CO2 forcing [J].
Wood, Tom ;
McKenna, Christine M. ;
Chrysanthou, Andreas ;
Maycock, Amanda C. .
ENVIRONMENTAL RESEARCH LETTERS, 2021, 16 (01)
[46]   Climate forcing due to optimization of maximal leaf conductance in subtropical vegetation under rising CO2 [J].
de Boer, Hugo Jan ;
Lammertsma, Emmy I. ;
Wagner-Cremer, Friederike ;
Dilcher, David L. ;
Wassen, Martin J. ;
Dekker, Stefan C. .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2011, 108 (10) :4041-4046
[47]   Why radiative forcing might fail as a predictor of climate change [J].
Stuber, N ;
Ponater, M ;
Sausen, R .
CLIMATE DYNAMICS, 2005, 24 (05) :497-510
[48]   Why radiative forcing might fail as a predictor of climate change [J].
Nicola Stuber ;
Michael Ponater ;
Robert Sausen .
Climate Dynamics, 2005, 24 :497-510
[49]   Climate Sensitivity and Feedbacks of a New Coupled Model CAMS-CSM to Idealized CO2 Forcing: A Comparison with CMIP5 Models [J].
Xiaolong Chen ;
Zhun Guo ;
Tianjun Zhou ;
Jian Li ;
Xinyao Rong ;
Yufei Xin ;
Haoming Chen ;
Jingzhi Su .
Journal of Meteorological Research, 2019, 33 :31-45
[50]   Climate Sensitivity and Feedbacks of a New Coupled Model CAMS-CSM to Idealized CO2 Forcing: A Comparison with CMIP5 Models [J].
Chen, Xiaolong ;
Guo, Zhun ;
Zhou, Tianjun ;
Li, Jian ;
Rong, Xinyao ;
Xin, Yufei ;
Chen, Haoming ;
Su, Jingzhi .
JOURNAL OF METEOROLOGICAL RESEARCH, 2019, 33 (01) :31-45