TY - JOUR
T1 - Impact of Ocean Eddy Resolution on the Sensitivity of Precipitation to CO2 Increase
AU - He, Jie
AU - Kirtman, Ben
AU - Soden, Brian J.
AU - Vecchi, Gabriel Andres
AU - Zhang, Honghai
AU - Winton, Michael
N1 - Funding Information:
This report was prepared by Jie He under award NA14OAR4320106 from the National Oceanic and Atmospheric Administration (NOAA), U.S. Department of Commerce. The statements, findings, conclusions, and recommendations are those of the authors and do not necessarily reflect the views of the National Oceanic and Atmospheric Administration or the U.S. Department of Commerce. We thank Liping Zhang and Xiaoqian Yan for their internal review at GFDL. Source codes of the models used in this paper are publically available (https://www.gfdl.noaa.gov/cm2-5-and-flor/). Simulations were conducted and archived on NOAA's computer clusters that belong to the U.S. government and are available from Jie He upon request.
Publisher Copyright:
©2018. The Authors.
PY - 2018/7/28
Y1 - 2018/7/28
N2 - The past few years have seen a growing investment in the development of global eddy-resolving ocean models, but the impact of incorporating such high ocean resolution on precipitation responses to CO2 forcing has yet to be investigated. This study analyzes precipitation changes from a suite of Geophysical Fluid Dynamics Laboratory models incorporating eddy-resolving (0.1°), eddy-permitting (0.25°), and eddy-parameterizing (1°) ocean models. The incorporation of eddy resolution does not challenge the large-scale structure of precipitation changes but results in substantial regional differences, particularly over ocean. These oceanic differences are primarily driven by the pattern of sea surface temperature (SST) changes with greater sensitivity in lower latitudes. The largest impact of ocean resolution on SST changes occurs in eddy-rich regions (e.g., boundary currents and the Southern Ocean), where impact on precipitation changes is also found to various degrees. In the Gulf Stream region where previous studies found considerable impact of eddy resolution on the simulation of climatological precipitation, we do not find such impact from the Geophysical Fluid Dynamics Laboratory models, but we do find substantial impact on precipitation changes. The eddy-parameterizing model projects a banded structure common to the Coupled Model Intercomparison Project (Phase 5) models, whereas the higher-resolution models project a poleward shift of precipitation maxima associated with an enhanced Gulf Stream warming. Over land, precipitation changes are generally not very sensitive to ocean resolution. In eastern North America adjacent to the Gulf Stream region, moderate differences are found between resolutions. We discuss the mechanisms of land differences, which arise through the simulation of both climatological SST and SST changes.
AB - The past few years have seen a growing investment in the development of global eddy-resolving ocean models, but the impact of incorporating such high ocean resolution on precipitation responses to CO2 forcing has yet to be investigated. This study analyzes precipitation changes from a suite of Geophysical Fluid Dynamics Laboratory models incorporating eddy-resolving (0.1°), eddy-permitting (0.25°), and eddy-parameterizing (1°) ocean models. The incorporation of eddy resolution does not challenge the large-scale structure of precipitation changes but results in substantial regional differences, particularly over ocean. These oceanic differences are primarily driven by the pattern of sea surface temperature (SST) changes with greater sensitivity in lower latitudes. The largest impact of ocean resolution on SST changes occurs in eddy-rich regions (e.g., boundary currents and the Southern Ocean), where impact on precipitation changes is also found to various degrees. In the Gulf Stream region where previous studies found considerable impact of eddy resolution on the simulation of climatological precipitation, we do not find such impact from the Geophysical Fluid Dynamics Laboratory models, but we do find substantial impact on precipitation changes. The eddy-parameterizing model projects a banded structure common to the Coupled Model Intercomparison Project (Phase 5) models, whereas the higher-resolution models project a poleward shift of precipitation maxima associated with an enhanced Gulf Stream warming. Over land, precipitation changes are generally not very sensitive to ocean resolution. In eastern North America adjacent to the Gulf Stream region, moderate differences are found between resolutions. We discuss the mechanisms of land differences, which arise through the simulation of both climatological SST and SST changes.
KW - Gulf Stream
KW - air-sea interaction
KW - high-resolution modeling
KW - ocean eddies
KW - precipitation changes
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U2 - 10.1029/2018GL078235
DO - 10.1029/2018GL078235
M3 - Article
AN - SCOPUS:85050366854
SN - 0094-8276
VL - 45
SP - 7194
EP - 7203
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 14
ER -