Wind-Driven Cross-Equatorial Flow in the Indian Ocean

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Wind-Driven Cross-Equatorial Flow in the Indian Ocean

Meridional velocity, mass, and heat transport in the equatorial oceans are difficult to estimate because of the nonapplicability of the geostrophic balance. For this purpose a steady-state model is utilized in the equatorial Indian Ocean using NCEP wind stress and temperature and salinity data from the World Ocean Atlas 2005 (WOA05) and Argo. The results show a Somali Current flowing to the sou...

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ژورنال

عنوان ژورنال: Journal of Physical Oceanography

سال: 2012

ISSN: 0022-3670,1520-0485

DOI: 10.1175/jpo-d-12-033.1