74:, or converging height lines near or above the level of non-divergence, which is near the 500 hPa pressure surface about midway up through the troposphere. On weather maps, high-pressure centers are associated with the letter H placed within the
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flow pattern in higher levels of the troposphere are beneath the western side of troughs. On weather maps, these areas show converging winds (isotachs), also known as
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with the highest pressure value. On constant pressure upper level charts, it is located within the highest height line contour.
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High-pressure systems form due to downward motion through the
121:"American Meteorological Society Glossary - Anticyclogenesis"
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42:. Anticyclones are alternatively referred to as
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187:The Weather Doctor. Retrieved on 2009-02-16.
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185:Weather's Highs and Lows: Part 1 The High.
22:is the development or strengthening of an
26:in the atmosphere. It is the opposite of
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127:from the original on 26 October 2006
30:(the dissolution or weakening of an
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66:occurs. Preferred areas within a
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196:Glossary of Meteorology (2009).
144:Glossary of Meteorology (2009).
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162:Middle-Latitude Cyclones - II.
123:. Allen Press Inc. June 2000.
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160:Konstantin Matchev (2009).
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183:Keith C. Heidorn (2005).
225:Meteorological phenomena
24:anticyclonic circulation
146:Level of nondivergence.
172:University of Florida
90: – Type of storm
44:high pressure systems
220:Atmospheric dynamics
38:equivalent known as
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131:2006-11-03
107:References
72:confluence
165:Archived
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82:See also
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