- Azores High
The Azores High, also known as the Bermuda High in the
United States , is a large subtropical semi-permanent centre of high atmospheric pressure found near theAzores in theAtlantic Ocean , at theHorse latitudes . It forms one pole of theNorth Atlantic oscillation , the other being theIcelandic Low . The system influences theweather and climatic patterns of vast areas ofNorth Africa andEurope . Thearid ity of theSahara Desert andMediterranean Basin is due to the subsidence of air in the system.In
summer , the central pressure lies around 1024mbar (hPa ), and moves north towards theIberian Peninsula , causing ridging acrossFrance , northernGermany and the southeasternUnited Kingdom . This brings hot and dry weather to these areas. In years that the Azores High is well developed, it extends westward towardBermuda , and begins to influence weather in theeastern United States . While it affects conditions in the western Atlantic, the Azores High can also be called the Bermuda High. Inwinter , the High moves to the south of the Azores, and fluctuations in pressure result in more variable weather.This high pressure block exhibits anticyclonic nature, circulating the air
clockwise . Due to this direction of movement, African eastern waves are impelled along the southern periphery of the Azores High away from coastalWest Africa towardsNorth America and theCaribbean , sometimes triggeringtropical cyclogenesis , especially during the hurricane season.ee also
*
Hadley cell
*North American High
*Siberian High
*South Atlantic High References
#cite web|url=http://www.weatheronline.co.uk/feature/aa030803.htm|title=The Azores High|accessdate=2006-11-19|work=WeatherOnline Weather facts
#cite web|url=http://amsglossary.allenpress.com/glossary/search?id=azores-high1|title=Azores high|accessdate=2006-11-19|work=Glossary of Meteorology|publisher=American Meteorological Society
#cite web|url=http://amsglossary.allenpress.com/glossary/search?id=bermuda-high1|title=Bermuda high|accessdate=2006-11-19|work=Glossary of Meteorology|publisher=American Meteorological Society
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