Validation of reanalysis Southern Ocean atmosphere trends using sea ice data

被引:13
|
作者
Hobbs, William R. [1 ,3 ,5 ]
Klekociuk, Andrew R. [2 ,3 ]
Pan, Yuhang [4 ]
机构
[1] Univ Tasmania, Inst Marine & Antarctic Studies IMAS, Hobart, Tas 7001, Australia
[2] Australian Antarctic Div, Antarct & Global Syst Program, 203 Channel Highway, Kingston, Tas 7050, Australia
[3] Univ Tasmania, IMAS, Australian Antarctic Program Partnership, Hobart, Tas 7001, Australia
[4] Univ Melbourne, Sch Earth Sci, McCoy Bldg, Parkville, Vic 3010, Australia
[5] Univ Tasmania, ARC Ctr Excellence Climate Extremes, IMAS, Hobart, Tas 7001, Australia
基金
澳大利亚研究理事会;
关键词
CLIMATE; RECONSTRUCTION; VARIABILITY; SHELVES; DRIVERS; HEAT;
D O I
10.5194/acp-20-14757-2020
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Reanalysis products are an invaluable tool for representing variability and long-term trends in regions with limited in situ data, and especially the Antarctic. A comparison of eight different reanalysis products shows large differences in sea level pressure and surface air temperature trends over the high-latitude Southern Ocean, with implications for studies of the atmosphere's role in driving ocean- sea ice changes. In this study, we use the established close coupling between sea ice cover and surface temperature to evaluate these reanalysis trends using the independent, 30-year sea ice record from 1980 to 2010. We demonstrate that sea ice trends are a reliable validation tool for most months of the year, although the sea ice-surface temperature coupling is weakest in summer when the surface energy budget is dominated by atmosphere-to-ocean heat fluxes. Based on our analysis, we find that surface air temperature trends in JRA55 are most consistent with satellite-observed sea ice trends over the polar waters of the Southern Ocean.
引用
收藏
页码:14757 / 14768
页数:12
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