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Intra-annual Variability of the Arabian Sea High Salinity Water Mass in the South-Eastern Arabian Sea during 2016-17

机译:2016-17年东南阿拉伯海阿拉伯海高盐度水团的年内变化

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摘要

Intra-annual variability of the Arabian Sea high salinity water mass (ASHSW) in the South Eastern Arabian Sea (SEAS) and Gulf of Mannar (GoM) are addressed in this paper by utilising the monthly missions carried out onboard INS Sagardhwani during 2016-17. Our observations revealed that the ASHSW was evident along the SEAS irrespective of seasons, whereas in the GoM the presence of ASHSW was observed during winter. The processes such as downwelling/up-welling, coastal currents, intrusion of low saline waters, stratification are clearly affect the spreading of the ASHSW. The characteristics such as core salinity value, depth and thickness of ASHSW exhibited remarkable spatio-temporal variability. Lateral mixing with the low saline waters in the region during winter reduces its core salinity. The intrusion of low saline waters was clearly seen upto 15 degrees N but the intrusion of low saline waters is not flowing through the GoM. The interface between the ASHSW and the prevailing low saline waters showed strong horizontal gradients of salinity. The presence of the ASHSW makes difference in the SLD and the below layer gradient which is sufficient to complicate or influence sound transmission. The spatio temporal variability of the ASHSW and its acoustic relevance are documented in this paper.
机译:本文利用2016-17年在萨加德瓦尼(INS Sagardhwani)上执行的月度任务来解决东南阿拉伯海(SEAS)和曼纳尔湾(GoM)的阿拉伯海高盐度水团(ASHSW)的年内变化问题。我们的观察结果表明,无论季节如何,ASHSW沿SEAS都很明显,而在GoM中,冬季观察到ASHSW的存在。向下涌流/向上涌流,沿海水流,低盐度水入侵,分层等过程显然会影响ASHSW的扩散。 ASHSW的岩心盐度值,深度和厚度等特征表现出显着的时空变化。在冬季,该地区与低盐度海水横向混合会降低其核心盐度。可以清楚地看到低盐度水的入侵在15度N以下,但低盐度水的入侵并未通过GoM。 ASHSW和盛行的低盐度水之间的界面显示出很强的盐度水平梯度。 ASHSW的存在使SLD和下层梯度有所不同,足以使声音传输复杂化或影响声音传输。本文记录了ASHSW的时空时空变化及其声学相关性。

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