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Pressure and Temperature structure of the atmosphere: • Pressure gradient controlled by ‘hydrostatic equilibrium’ — pressure supports weight of gas above it, and, because it is gas, density drops with decreasing
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Document Date: 2014-12-10 12:58:09
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File Size: 1,44 MB
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Iceland /
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Event
Natural Disaster /
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IndustryTerm
e-folding /
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SocialTag
Atmospheric dynamics
Atmosphere
Tropical meteorology
Intertropical Convergence Zone
Low-pressure area
Coriolis effect
Atmosphere of Earth
Troposphere
Benoît Paul Émile Clapeyron
Atmospheric sciences