The NECC is a direct response to the meridional change of the wind stress curl near the Intertropical Convergence Zone ( ITCZ ).
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However, upon entering a shallow, gently sloping shelf, the surge cannot be dispersed, but is driven ashore by the wind stresses of the hurricane.
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The wind stress also generates turbulence, which causes the surface fresh water to be mixed down and results in a brackish layer typically thick.
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The NECC is an interesting case because while it results from wind-driven circulation, it transports water against the mean westward wind stress in the tropics.
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The areas of most positive wind stress curl are characterized by very weak sea surface temperature incline, and are likely consistent to regions of mode water.
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A . Storm surge : A rise of water above normal level along a shore due to the action of wind stress on the water surface.
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The AMOC is calculated on the basis of the directly measured boundary currents, the geostrophic currents and the Ekman transports estimated from the surface wind stress.
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Some work had already been carried out by Eug�ne Viollet-Le-Duc, but he had died in 1879 . Eiffel was selected because of his experience with wind stresses.
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The wind-driven horizontal transport in the mixed layer is approximately described by Ekman Layer dynamics in which vertical diffusion of momentum balances the Coriolis effect and wind stress.
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This apparent paradox is concisely explained by Sverdrup theory, which shows that the east-west transport is governed by the north-south change in the curl of the wind stress.
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