Seasonal and Interannual Variability of the Subtropical South Indian Ocean Sea Surface Salinity Maximum

被引:1
作者
Bingham, F. M. [1 ]
Brodnitz, S. K. [1 ]
Gordon, A. L. [2 ]
机构
[1] Univ North Carolina Wilmington, Ctr Marine Sci, Wilmington, NC 28403 USA
[2] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA
关键词
salinity; evaporation; precipitation; subtropical gyre; South Indian Ocean; PACIFIC TROPICAL WATER; MIXED-LAYER SALINITY; CIRCULATION; CYCLE; DISTRIBUTIONS; TEMPERATURE; AQUARIUS; CURRENTS; IMPACTS; ARGO;
D O I
10.1029/2022JC018982
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The sea surface salinity (SSS) maximum of the South Indian Ocean (the SISSS-max) is a high-salinity feature centered at 30 & DEG;S, 90 & DEG;E, near the center of the South Indian subtropical gyre. It is located poleward of a region of strong evaporation and weak precipitation. Using several different satellites and in situ data sets, we track changes in this feature since the early 2000s. The centroid of the SISSS-max moves seasonally north and south, furthest north in late winter and farthest south in late summer. Interannually, the SISSS-max has moved on a northeast-southwest path about 1,500 km in length. The size and maximum SSS of the feature vary in tandem with this motion. It gets larger (smaller) and saltier (fresher) as it moves to the northeast (southwest) closer to (further from) the area of strongest surface freshwater flux. The area of the SISSS-max almost doubles from its smallest to largest extent. It was maximum in area in 2006, decreased steadily until it reached a minimum in 2013, and then increased again. The seasonal variability of the SISSS-max is controlled by the changes that occur on its poleward, or southern, side, whereas interannual variability is controlled by changes on its equatorward side. The variations in the SISSS-max are a complex dance between changes in evaporation, precipitation, wind forcing, gyre-scale ocean circulation, and downward Ekman pumping. Its motion correlated with SSS changes throughout the South Indian Ocean and may be an indicator of changes in the basin's subtropical circulation.
引用
收藏
页数:15
相关论文
共 55 条
[1]  
Berger M, 2002, ESA BULL-EUR SPACE, P113
[2]   Sea Surface Salinity Subfootprint Variability from a Global High-Resolution Model [J].
Bingham, Frederick M. ;
Brodnitz, Susannah ;
Fournier, Severine ;
Ulfsax, Karly ;
Hayashi, Akiko ;
Zhang, Hong .
REMOTE SENSING, 2021, 13 (21)
[3]   Variability of the South Pacific Subtropical Surface Salinity Maximum [J].
Bingham, Frederick M. ;
Busecke, Julius J. M. ;
Gordon, Arnold L. .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2019, 124 (08) :6050-6066
[4]   The North Atlantic subtropical surface salinity maximum as observed by Aquarius [J].
Bingham, Frederick M. ;
Busecke, Julius ;
Gordon, Arnold L. ;
Giulivi, Claudia F. ;
Li, Zhijin .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2014, 119 (11) :7741-7755
[5]   Linear trends in salinity for the World Ocean, 1955-1998 [J].
Boyer, TP ;
Levitus, S ;
Antonov, JI ;
Locarnini, RA ;
Garcia, HE .
GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (01) :1-4
[6]   A subtropical North Atlantic regional atmospheric moisture budget [J].
D'Addezio, Joseph M. ;
Bingham, Frederick M. .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2014, 119 (12) :8731-8748
[7]   Arterial ocean circulation of the southeast Indian Ocean [J].
Divakaran, Prasanth ;
Brassington, Gary B. .
GEOPHYSICAL RESEARCH LETTERS, 2011, 38
[8]   The Freshwater Balance Over the North Atlantic SPURS Domain from Aquarius Satellite Salinity, OSCAR Satellite Surface Currents, and Some Simplified Approaches [J].
Dohan, Kathleen ;
Kao, Hsun-Ying ;
Lagerloef, Gary S. E. .
OCEANOGRAPHY, 2015, 28 (01) :86-95
[9]   Mixed-Layer Salinity Budget in the SPURS Region on Seasonal to Interannual Time Scales [J].
Dong, Shenfu ;
Goni, Gustavo ;
Lumpkin, Rick .
OCEANOGRAPHY, 2015, 28 (01) :78-85
[10]   Fifty-Year Trends in Global Ocean Salinities and Their Relationship to Broad-Scale Warming [J].
Durack, Paul J. ;
Wijffels, Susan E. .
JOURNAL OF CLIMATE, 2010, 23 (16) :4342-4362