{"id":1185,"date":"1999-11-30T00:00:00","date_gmt":"1999-11-30T05:00:00","guid":{"rendered":"https:\/\/setsail.com\/?p=1185"},"modified":"2015-10-16T12:15:05","modified_gmt":"2015-10-16T17:15:05","slug":"sea-breeze-effects","status":"publish","type":"post","link":"https:\/\/setsail.com\/sea-breeze-effects\/","title":{"rendered":"Sea Breeze Effects"},"content":{"rendered":"
Steve, My question relates to how the sea and land temperatures influence wind patterns. If the sea temperature is warmer than the adjacent land, then what type of flow can I expect? This specifically relates to So. Calif. waters and down towards Ensenada. Thanks, John <\/p>\n<\/div>\n
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At night the process often reverses, with the cooler land air descending and flowing out over the now warmer ocean.<\/p>\n
So, in S. California and along the Baja coast this is why you get an afternoon onshore (sea breeze) flow – which often reverses some time after midnight through the early morning hours.<\/p>\n
To the extent that there is a pressure gradient present exclusive of the temperature differential, the sea breeze or night time land breeze, will reinforce the gradient or reduce it.<\/p>\n
There is an entire section in our Mariner’s Weather Handbook which goes into this in great detail.<\/p>\n
Steve<\/p>\n
PS-differentials in sea temperature, especially in areas like the Gulf Stream or South Australian current also have a big impact on local weather. <\/p>\n
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