Dynamics of ocean surface mixed layer variability in the Indian Ocean

被引:23
作者
Schiller, Andreas [1 ]
Oke, Peter R. [1 ]
机构
[1] Ctr Australian Weather & Climate Res, CSIRO Oceans & Atmosphere Flagship, Hobart, Tas, Australia
关键词
Indian Ocean; mixed layer; heat budget; salinity budget; TROPICAL WESTERN PACIFIC; FRESH-WATER DISCHARGE; INTRASEASONAL VARIABILITY; THERMAL STRUCTURE; HEAT-BALANCE; ARABIAN SEA; TEMPERATURE; CIRCULATION; BUDGET; SCALE;
D O I
10.1002/2014JC010538
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
We present a new methodology that allows quantifying the impact of individual terms of the temperature and salinity conservation within the mixed layer on mixed layer depth (MLD). The method is applied to output from an ocean general circulation model in the Indian Ocean to investigate variability and changes in MLD. On seasonal timescales and for most areas of the Indian Ocean variability of MLD is tightly linked to all thermohaline budget terms. In the Indian Ocean at approximately 20 degrees S the MLD covaries with surface heat and freshwater fluxes on intraseasonal and interannual timescales. The geography of the region includes the Leeuwin Current, plus the tropical eastern Indian Ocean for interannual surface freshwater fluxes. The range of seasonal amplitudes of MLD variability varies with individual budget terms but is typically within 1 m/month to 100 m/month. The ocean footprints of an intraseasonal tropical cyclone, tropical and midlatitude seasonal temperature and salinity budgets and interannual variability associated with the Indian Ocean Dipole Mode are analyzed. The results reveal close relationships of the thermohaline budgets within the mixed layer with the variability of the MLD. The associated tendencies of changes in MLD are consistent with Argo and satellite-based observations of tendencies within the mixed layer and sea-surface temperature and salinity.
引用
收藏
页码:4162 / 4186
页数:25
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