Titlebook: Observations and Dynamics of Circulations in the North Indian Ocean; Julian P. McCreary,Satish R. Shetye Textbook 2023 The Editor(s) (if a

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Sverdrup Flow and Boundary Currentsundamental response is now called a “Sverdrup flow” and the balance of terms that generates it a “Sverdrup balance.” A mode of the LCS model can also be in a state of Sverdrup balance, and it is useful to refer to that response as also being a Sverdrup flow. In response to forcing by zonal winds, Sv

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Interior Oceannal momentum equations. When the wind is switched on, the Coriolis parameter . is constant, and there is no vertical diffusion, Ekman flow continuously drains (piles up) water to the left (right) of the wind axis in the northern hemisphere, and vice versa in the southern hemisphere, a process known

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Equatorial Ocean: Switched-On Forcingg terms in the meridional momentum equation (the “long-wavelength” approximation). They are found under the assumption that the Coriolis parameter is given by ., allowing them to be represented as expansions in Hermite functions. In an unbounded ocean, Ekman drift and Ekman pumping quickly establish

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GUMP

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Atmospheric Circulationquence of these interactions is that during summer the Bay of Bengal becomes the most active region of the global ITCZ. Superimposed on the climatological-mean annual cycle is variability at interannual and sub-annual time scales, with amplitudes as large as that of the annual cycle itself.

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