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DOI10.1029/2019MS001870
The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution
Caldwell P.M.; Mametjanov A.; Tang Q.; Van Roekel L.P.; Golaz J.-C.; Lin W.; Bader D.C.; Keen N.D.; Feng Y.; Jacob R.; Maltrud M.E.; Roberts A.F.; Taylor M.A.; Veneziani M.; Wang H.; Wolfe J.D.; Balaguru K.; Cameron-Smith P.; Dong L.; Klein S.A.; Leung L.R.; Li H.-Y.; Li Q.; Liu X.; Neale R.B.; Pinheiro M.; Qian Y.; Ullrich P.A.; Xie S.; Yang Y.; Zhang Y.; Zhang K.; Zhou T.
发表日期2019
ISSN19422466
起始页码4095
结束页码4146
卷号11期号:12
英文摘要This study provides an overview of the coupled high-resolution Version 1 of the Energy Exascale Earth System Model (E3SMv1) and documents the characteristics of a 50-year-long high-resolution control simulation with time-invariant 1950 forcings following the HighResMIP protocol. In terms of global root-mean-squared error metrics, this high-resolution simulation is generally superior to results from the low-resolution configuration of E3SMv1 (due to resolution, tuning changes, and possibly initialization procedure) and compares favorably to models in the CMIP5 ensemble. Ocean and sea ice simulation is particularly improved, due to better resolution of bathymetry, the ability to capture more variability and extremes in winds and currents, and the ability to resolve mesoscale ocean eddies. The largest improvement in this regard is an ice-free Labrador Sea, which is a major problem at low resolution. Interestingly, several features found to improve with resolution in previous studies are insensitive to resolution or even degrade in E3SMv1. Most notable in this regard are warm bias and associated stratocumulus deficiency in eastern subtropical oceans and lack of improvement in El Niño. Another major finding of this study is that resolution increase had negligible impact on climate sensitivity (measured by net feedback determined through uniform +4K prescribed sea surface temperature increase) and aerosol sensitivity. Cloud response to resolution increase consisted of very minor decrease at all levels. Large-scale patterns of precipitation bias were also relatively unaffected by grid spacing. ©2019. The Authors.
语种英语
scopus关键词Mean square error; Sea ice; Surface waters; Climate sensitivity; Control simulation; Earth system model; High resolution simulations; Initialization procedures; Resolution increase; Root mean squared errors; Sea surface temperature (SST); Ocean currents; aerosol; climate change; climate effect; climate forcing; climate modeling; CMIP; ensemble forecasting; sea ice; sea surface temperature; spatial resolution; stratocumulus; Atlantic Ocean; Labrador Sea
来源期刊Journal of Advances in Modeling Earth Systems
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/156816
作者单位Lawrence Livermore National Lab, Livermore, CA, United States; Argonne National Laboratory, Lemont, IL, United States; Los Alamos National Laboratory, Los Alamos, NM, United States; Brookhaven National Laboratory, Upton, NY, United States; Lawrence Berkeley National Laboratory, Berkeley, CA, United States; Sandia National Laboratories, Albuquerque, NM, United States; Pacific Northwest National Laboratory, Richland, WA, United States; Department of Civil and Environmental Engineering, University of Houston, Houston, TX, United States; Department of Atmospheric Science, University of  Wyoming, Laramie, WY, United States; National Center for Atmospheric Research, Boulder, CO, United States; Department of Land, Air, and Water Resources, University of California-Davis, Davis, CA, United States
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Caldwell P.M.,Mametjanov A.,Tang Q.,et al. The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution[J],2019,11(12).
APA Caldwell P.M..,Mametjanov A..,Tang Q..,Van Roekel L.P..,Golaz J.-C..,...&Zhou T..(2019).The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution.Journal of Advances in Modeling Earth Systems,11(12).
MLA Caldwell P.M.,et al."The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution".Journal of Advances in Modeling Earth Systems 11.12(2019).
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