Research Article

Ekman Pumping and Mixed Layer Depth Variability over the Indo-Pacific Oceans during the El Nino and IOD Events  

Veeranjaneyulu Ch.1 , A. A. Deo2 , G.  Bharathi1 , D. W.  Ganer2 , Prasad  K. V. S. R.1
1. Department of Meteorology and Oceanography, Andhra University, Visakhapatnam-530003, India
2. Indian Institute of Tropical Meteorology, Pune, India-411008
Author    Correspondence author
International Journal of Marine Science, 2016, Vol. 6, No. 56   doi: 10.5376/ijms.2016.06.0056
Received: 02 Nov., 2016    Accepted: 19 Dec., 2016    Published: 20 Dec., 2016
© 2016 BioPublisher Publishing Platform
This is an open access article published under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Preferred citation for this article:

Veeranjaneyulu Ch., Deo A.A, Bharathi G., Ganer D.W., and Prasad K.V.S.R., 2016, Ekman Pumping and Mixed Layer Depth Variability over the Indo-Pacific Oceans during the El Nino and IOD Events, International Journal of Marine Science, 6(56):1-9 (doi: 10.5376/ijms.2016.06.0056)

Abstract

The following study addresses the variability of Mixed Layer Depth (MLD) and Ekman pumping (WEK) during the extreme El Nino and Indian Ocean Dipole (IOD) over the Indo-Pacific regions. Monthly anomalies considering the climatology of the period of 1980 through 2011 show that during the El Nino years, Ekman suction (positive Ekman pumping) is replaced with Ekman pumping (negative Ekman pumping) in the tropical eastern Pacific Ocean (88˚W-90˚W and 13˚S-15˚S) resulting in positive MLD anomalies, and the strong Ekman pumping may be the source for the deepened thermocline during El Nino. In the La Nina events shallow MLD exits in the tropical eastern Pacific Ocean, due to positive Ekman pumping. During the positive IOD (PIOD) events in the south eastern Indian Ocean (97˚E-100˚E and 2˚S-5˚S) MLD becomes shallow and positive Ekman pumping anomalies occur. During the negative IOD (NIOD) years opposite signs take place. Composite events of El Nino are compared with those of IOD, showing more Ekman pumping anomalies during IOD events as against less deviation in SST.

Keywords
Ekman pumping; Mixed layer depth; El Nino and La Nina; IOD
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International Journal of Marine Science
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