Diagnostics for near-surface wind response to the Gulf Stream in a regional atmospheric model

The diagnostics for the surface-layer momentum vector, its curl, and its convergence are developed with a clear separation of pressure adjustment from downward momentum inputs from aloft in the surface layer system. The results suggest that the downward momentum mixing mechanism plays a dominant role contributing to the annual-mean climatological momentum curl, whereas the pressure adjustment mechanism plays a minor role.

In contrast, the wind convergence is mainly due to the pressure adjustment mechanism. This can be explained by the orientation of background wind to the sea surface temperature front. The diagnostics also explain the relatively strong seasonal variation in surface-layer momentum convergence and the small seasonal variation in curl.