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wind-driven current

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wind-driven current [′win ¦driv·ən ′kə·rənt]
(oceanography)


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Whilst the currents in continental shelf seas, like the Irish Sea and North Sea, are dominated by the tide, there is evidence that much weaker wind-driven currents might be responsible for circulating key nutrients within the seas.
Geological Survey says the low oxygen levels may result from wind-driven currents.
A new study suggests that these enigmatic waters expand when their permafrost banks melt, rather than when wind-driven currents cause erosion, as scientists had proposed for decades.
 
 
 
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