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Title: Intermodel Spread in the Pattern Effect and Its Contribution to Climate Sensitivity in CMIP5 and CMIP6 Models

Journal Article · · Journal of Climate
ORCiD logo [1];  [1];  [2];  [3];  [1];  [4];  [5]
  1. Univ. of Washington, Seattle, WA (United States)
  2. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
  3. Univ. of Illinois at Urbana-Champaign, IL (United States)
  4. Nanjing Univ. (China)
  5. Met Office Hadley Centre, Exeter (United Kingdom)

Radiative feedbacks depend on the spatial patterns of sea surface temperature (SST) and thus can change over time as SST patterns evolve—the so-called pattern effect. In this study, we investigate intermodel differences in the magnitude of the pattern effect and how these differences contribute to the spread in effective equilibrium climate sensitivity (ECS) within CMIP5 and CMIP6 models. Effective ECS in CMIP5 estimated from 150-yr-long abrupt4×CO2 simulations is on average 10% higher than that estimated from the early portion (first 50 years) of those simulations, which serves as an analog for historical warming; this difference is reduced to 7% on average in CMIP6. The (negative) net radiative feedback weakens over the course of the abrupt4×CO2 simulations in the vast majority of CMIP5 and CMIP6 models, but this weakening is less dramatic on average in CMIP6. For both ensembles, the total variance in the effective ECS is found to be dominated by the spread in radiative response on fast time scales, rather than the spread in feedback changes. Using Green’s functions derived from two AGCMs shows that the spread in feedbacks on fast time scales may be primarily due to differences in atmospheric model physics, whereas the spread in feedback evolution is primarily governed by differences in SST patterns. Intermodel spread in feedback evolution is well explained by differences in the relative warming in the West Pacific warm-pool regions for the CMIP5 models, but this relation fails to explain differences across the CMIP6 models, suggesting that a stronger sensitivity of extratropical clouds to surface warming may also contribute to feedback changes in CMIP6.

Research Organization:
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE National Nuclear Security Administration (NNSA); National Science Foundation (NSF); National Natural Science Foundation of China (NSFC)
Grant/Contract Number:
AC52-07NA27344; AGS-1752796; NSFC 41875095
OSTI ID:
1658691
Report Number(s):
LLNL-JRNL-800377; 1003695
Journal Information:
Journal of Climate, Vol. 33, Issue 18; ISSN 0894-8755
Publisher:
American Meteorological SocietyCopyright Statement
Country of Publication:
United States
Language:
English

References (39)

The Dependence of Global Cloud and Lapse Rate Feedbacks on the Spatial Structure of Tropical Pacific Warming journal January 2018
The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate Models journal February 2015
Energy budget constraints on climate sensitivity in light of inconstant climate feedbacks journal April 2017
Time-Varying Climate Sensitivity from Regional Feedbacks journal July 2013
Feedback temperature dependence determines the risk of high warming: FEEDBACK TEMPERATURE DEPENDENCE journal June 2015
Forcing and feedback in the MPI-ESM-LR coupled model under abruptly quadrupled CO 2 : FORCING AND FEEDBACK IN THE MPI-ESM-LR journal October 2013
Strong Dependence of Atmospheric Feedbacks on Mixed‐Phase Microphysics and Aerosol‐Cloud Interactions in HadGEM3 journal June 2019
Marine boundary layer clouds at the heart of tropical cloud feedback uncertainties in climate models journal January 2005
How Well Do We Understand and Evaluate Climate Change Feedback Processes? journal August 2006
State-dependent climate sensitivity in past warm climates and its implications for future climate projections journal August 2013
Quantifying the Sources of Intermodel Spread in Equilibrium Climate Sensitivity journal January 2016
Evaluating Emergent Constraints on Equilibrium Climate Sensitivity journal May 2018
Potential Problems Measuring Climate Sensitivity from the Historical Record journal March 2020
Attributing Historical and Future Evolution of Radiative Feedbacks to Regional Warming Patterns using a Green’s Function Approach: The Preeminence of the Western Pacific journal September 2019
An Assessment of the Primary Sources of Spread of Global Warming Estimates from Coupled Atmosphere–Ocean Models journal October 2008
High Climate Sensitivity in the Community Earth System Model Version 2 (CESM2) journal July 2019
The DOE E3SM Coupled Model Version 1: Overview and Evaluation at Standard Resolution journal July 2019
Quantifying climate feedbacks in polar regions journal May 2018
A new method for diagnosing radiative forcing and climate sensitivity journal January 2004
How accurately can the climate sensitivity to $$\hbox {CO}_{2}$$CO2 be estimated from historical climate change? journal October 2019
Relative roles of surface temperature and climate forcing patterns in the inconstancy of radiative feedbacks: Inconstancy of Radiative Feedbacks journal July 2017
On the pattern of CO 2 radiative forcing and poleward energy transport : CO journal October 2017
Exposing Global Cloud Biases in the Community Atmosphere Model (CAM) Using Satellite Observations and Their Corresponding Instrument Simulators journal August 2012
The Impact of Recent Forcing and Ocean Heat Uptake Data on Estimates of Climate Sensitivity journal August 2018
Implications for climate sensitivity from the response to individual forcings journal December 2015
Internal Variability and Disequilibrium Confound Estimates of Climate Sensitivity From Observations journal February 2018
Robust increase in equilibrium climate sensitivity under global warming: ROBUST INCREASE IN CLIMATE SENSITIVITY journal November 2013
The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6 journal January 2016
Slow climate mode reconciles historical and model-based estimates of climate sensitivity journal July 2017
UKESM1: Description and Evaluation of the U.K. Earth System Model journal December 2019
The Diversity of Cloud Responses to Twentieth Century Sea Surface Temperatures journal January 2018
An Assessment of Climate Feedbacks in Coupled Ocean–Atmosphere Models journal July 2006
Prospects for narrowing bounds on Earth's equilibrium climate sensitivity: EARTH'S EQUILIBRIUM CLIMATE SENSITIVITY journal November 2016
Cloud Phase Changes Induced by CO2 Warming—a Powerful yet Poorly Constrained Cloud-Climate Feedback journal October 2015
Importance of the mixed-phase cloud distribution in the control climate for assessing the response of clouds to carbon dioxide increase: a multi-model study journal April 2006
On the contribution of local feedback mechanisms to the range of climate sensitivity in two GCM ensembles journal February 2006
The impact of parametrized convection on cloud feedback
  • Webb, Mark J.; Lock, Adrian P.; Bretherton, Christopher S.
  • Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, Vol. 373, Issue 2054 https://doi.org/10.1098/rsta.2014.0414
journal November 2015
Impact of decadal cloud variations on the Earth’s energy budget journal October 2016
Analyzing the dependence of global cloud feedback on the spatial pattern of sea surface temperature change with a G reen's function approach journal September 2017

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