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Yanai waves in the western equatorial Indian Ocean

Chatterjee, A and Shankar, D and McCreary, JP and Vinayachandran, PN (2013) Yanai waves in the western equatorial Indian Ocean. In: Journal of Geophysical Research: Oceans, 118 (3). pp. 1556-1570.

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Official URL: http://dx.doi.org/10.1002/jgrc.20121

Abstract

Observations and models have shown the presence of intraseasonal fluctuations in 20-30-day and 10-20-day bands in the equatorial Indian Ocean west of 60 degrees E (WEIO). Their spatial and temporal structures characterize them as Yanai waves, which we label low-frequency (LFYW) and high-frequency (HFYW) Yanai waves, respectively. We explore the dynamics of these intraseasonal signals, using an ocean general circulation model (Modular Ocean Model) and a linear, continuously stratified model. Yanai waves are forced by the meridional wind tau(y) everywhere in the WEIO most strongly during the monsoon seasons. They are forced both directly in the interior ocean and by reflection of the interior response from the western boundary; interference between the interior and boundary responses results in a complex surface pattern that propagates eastward and has nodes. Yanai waves are also forced by instabilities primarily during June/July in a region offshore from the western boundary (52-55 degrees E). At that time, eddies, generated by barotropic instability of the Southern Gyre, are advected southward to the equator. There, they generate a westward-propagating, cross-equatorial flow field, v(eq), with a wave number/frequency spectrum that fits the dispersion relation of a number of Yanai waves, and these waves are efficiently excited. Typically, Yanai waves associated with several baroclinic modes are excited by both wind and eddy forcing; and typically, they superpose to create beams that carry energy vertically and eastward along ray paths. The same processes generate LFYWs and HFYWs, and hence, their responses are similar; differences are traceable to the property that HFYWs have longer wavelengths than LFYWs for each baroclinic mode.

Item Type: Journal Article
Additional Information: Copyright of this article belongs to American Geophysical Union.
Keywords: Yanai Waves; Equatorial Dynamics; Indian Ocean; Instability; Energetics
Department/Centre: Division of Mechanical Sciences > Centre for Atmospheric & Oceanic Sciences
Depositing User: Francis Jayakanth
Date Deposited: 06 Aug 2013 11:43
Last Modified: 06 Aug 2013 11:43
URI: http://eprints.iisc.ac.in/id/eprint/46920

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