The Gulf Stream is linked to causing high winds so why are our local winds often so weak?
Well we often have high winds during the winter season here in Jacksonville especially when strong high pressure ridges move off the mid Atlantic and generate local Nor’easters. The First Coast and the southeast United States in general, are located in an area of relatively lighter wind patterns. Due to the proximity of the Bermuda Ridge.
A recent climatology mapping sea winds using QuickSCAT has been completed by Takeaki Sampe and Shang-Ping Xie, highlights areas of strong winds over the globe. High winds are most likely in the North Atlantic in midwinter. The colors in this image show the percent of high winds over 45 mph. Stronger winds are red and yellow. Notice how the high winds are located off the northeast US and Canadian Maritimes. This is the location of the average mid-latitude jet stream that drives strong storms over the area. But the Gulf Stream plays a major role in increasing the high winds. It causes a gradient of warm and cold water called static instability. This contrast results in vertical turbulent mixing of the air. Gusty winds aloft dives down to the surface to replace warmer lighter air. This acceleration of the surface wind is maximized along the northern wall of the Gulf Stream where it branches east into the Atlantic current.

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