User:Dasani34/Sample page

Welcome to Wikipedia! This page is a sandbox, an area where you can experiment and test edits. It contains simple examples of various elements you'll find around Wikipedia. It may be deleted after a period of inactivity; please do not use it to draft an article or create anything else you wish to last.

Wind-Stress Curl


Wind-stress curl is a spatial gradient in wind speed. It has a significant influence on coastal upwelling and downwelling. Wind-stress curl occurs when there is a strong longshore wind that is adjacent to a weaker wind. Ekman transport from the stronger wind would push surface water eastward or westward (depending on the location being observed), but the weaker wind would be pushing the surface water at a much slower rate. This difference in speed would cause the water to either converge or diverge. Positive wind-stress curl results in upwelling and negative wind-stress curl results in downwelling.