Estimating the global oceanic net freshwater flux from Argo and comparing it with satellite-based freshwater flux products

被引:11
|
作者
Ren, Li [1 ,2 ]
Hackert, Eric [3 ]
Arkin, Phillip [1 ]
Busalacchi, Antonio J. [3 ]
机构
[1] Univ Maryland, ESSIC CICS, College Pk, MD 20742 USA
[2] NOAA NESDIS STAR SOCD, College Pk, MD USA
[3] Univ Maryland, ESSIC, College Pk, MD 20742 USA
基金
美国国家科学基金会;
关键词
salt budget; oceanic precipitation; oceanic evaporation; SURFACE-LAYER SALINITY; PROBABILITY-DISTRIBUTION FUNCTIONS; TROPICAL PACIFIC-OCEAN; GAUGE OBSERVATIONS; MIXED-LAYER; PRECIPITATION; MODEL; CYCLE; BUDGET; GPCP;
D O I
10.1002/2013JC009620
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Following the idea that analysis of in situ information in the salt budget could be used as a surrogate for global ocean rain gauge, the annual mean oceanic net freshwater flux (E-P) was estimated from the Argo profiles and the wind stress data on a global scale. The comparison between the independent E-P estimation from Argo and the E-P product sets, including the combination of precipitation from TRMM, GPCP, CMAP and evaporation from OAFlux, GSSTF3 and IFREMER and E-P set from NEWS formed from satellite, generally show similar spatial patterns, particularly on the large scale. However, there are differences among the different satellite-based E-P estimates and between satellite estimates and independent in situ estimates. Based on the pattern correlation and the RMSD, the evaporation and precipitation from OAFlux and TRMM agrees best with the E-P estimated from the independent Argo-based estimates.
引用
收藏
页码:7869 / 7881
页数:13
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