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ISSN : 2332-2594

Journal of Climatology & Weather Forecasting
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Research Article

Sea Surface Temperature and Find Later Jet Variations over Arabian Sea During Summer Monsoon

M. V. Subrahmanyam1*, K.P.R. Vittal Murty2 and B.Pushpanjali2
1Marine Science Department, Zhejiang Ocean University, Zhoushan, Zhejiang, China
2Department of Environmental Sciences, Acharya Nagarjuna University, Guntur, AP, India
Corresponding Author : Subrahmanyam MV
Marine Science Department, Zhejiang Ocean University
Zhoushan, Zhejiang, China
Tel: +86-18368086386
E-mail: [email protected]
Received February 25, 2014; Accepted June 10, 2014; Published June 17, 2014
Citation: M. V. Subrahmanyam, K.P.R. Vittal Murty, B.Pushpanjali (2014) Sea Surface Temperature and Find Later Jet Variations over Arabian Sea During Summer Monsoon. J Climatol Weather Forecasting 2:111. doi:10.4172/2332-2594.1000111
Copyright: © 2014 Subrahmanyam MV et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
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Abstract

Indian summer monsoon is important to study in relation with the air-sea interaction processes. Find later jet (FLJ) is a Low Level Jet observed at 850 mb by which the moisture is transported to the Indian sub-continent from the Indian Ocean. In this connection it is important to observe FLJ intensity variations over Arabian Sea. In this article authors attempted to examine the Intraseasonal variability of FLJ intensities for the period 1980-2012 in relation to Sea Surface Temperature anomalies (SSTA) over Arabian Sea during summer monsoon season. As El Nino and La Nina are affecting the summer monsoon rainfall, authors studied the variations in FLJ and SSTA and also evaluated the correlation between FLJ and SSTA during the above mentioned period. An apparent relationship is found between the intensity of FLJ and SSTA over Arabian Sea region. FLJ is increasing in July during an El Nino event and SSTA is higher positive anomalies.

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