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The atmospheric pressure decreases rapidly with height in the lower atmosphere, dropping about 1 mb for every 10 m increase in elevation. Small differences in pressure are significant for wind patterns. Low and high pressure systems are surrounded by isobars with the lowest/highest pressure at the center. Near the equator pressure is low, forming the equatorial low, while 30°N/S feature subtropical highs and 60°N/S have subpolar lows, with polar highs near the poles. Winds result from the interaction of pre

Author

Ankit

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EN