Observed year-to-year sea surface salinity variability in the Bay of Bengal during the 2009–2014 period

被引:1
|
作者
Akurathi Venkata Sai Chaitanya
Fabien Durand
Simi Mathew
Vissa Venkata Gopalakrishna
Fabrice Papa
Matthieu Lengaigne
Jerome Vialard
Chanda Kranthikumar
R. Venkatesan
机构
[1] CSIR/National Institute of Oceanography (NIO),Indo
[2] IRD/Laboratoire d’études en Géophysique et Océanographie Spatiales (LEGOS),French Cell for Water Sciences
[3] Indo-French Cell for Water Sciences,undefined
[4] IISc-NIO-IITM–IRD Joint International Laboratory,undefined
[5] IISc,undefined
[6] National Institute of Ocean Technology (NIOT),undefined
[7] Sorbonne Universités,undefined
[8] UPMC Univ Paris 06,undefined
[9] UMR 7159,undefined
[10] LOCEAN,undefined
[11] National Institute of Oceanography,undefined
来源
Ocean Dynamics | 2015年 / 65卷
关键词
SSS; Bay of Bengal; Argo; Ganges; Brahmaputra; IOD;
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学科分类号
摘要
The present study describes the observed sea surface salinity (SSS) interannual variability in the Bay of Bengal over the 2009–2014 period. It is based on an original compilation of all available in situ SSS observations in that region, assembled in a 2°-resolution trimonthly gridded field. We find that year-to-year SSS variability is particularly strong in the north-eastern part of the bay. Over recent years, this variability takes the form of two successive and opposite phases: a saltening phase from mid-2009 to late 2010, immediately followed by a freshening phase from late 2010 to late 2011. The typical magnitude of each anomalous spell is about one in the practical salinity scale, making this area one of the most variable of the tropical oceans at interannual timescales. A simple mixed-layer salt budget indicates that year-to-year large-scale SSS variability in the Northern Bay of Bengal is primarily driven by freshwater flux variability with a correlation of 0.68, with rather independent contributions from precipitation and river run-off. The oceanic surface circulation variability contributes less systematically to the large-scale SSS evolution in the Northern Bay of Bengal over the entire record with a correlation of 0.13, despite a strong contribution at times, in particular, during the 2011 positive Indian Ocean Dipole (IOD) freshening.
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页码:173 / 186
页数:13
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