Abstract
Monthly wind stress contoured for the western Indian Ocean clearly shows the SW monsoon from May through September to be considerably stronger than the NE monsoon with a maximum in January. Maps of wind stress curl during the SW monsoon show a large region of negative curl to the NE off the Somali coast, whereas a region of high positive curl occurs off the Arabian coast and in a small band off the Somali east coast north of 5oN.-after Author
Cite
CITATION STYLE
Bruce, J. G. (1983). The wind field in the western Indian Ocean and the related ocean circulation. Monthly Weather Review, 111(7), 1442–1452. https://doi.org/10.1175/1520-0493(1983)111<1442:TWFITW>2.0.CO;2
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