![Atmospheric dynamics / Atmosphere / Tropical meteorology / Intertropical Convergence Zone / Low-pressure area / Coriolis effect / Atmosphere of Earth / Troposphere / Benoît Paul Émile Clapeyron / Atmospheric sciences / Meteorology / Atmospheric thermodynamics Atmospheric dynamics / Atmosphere / Tropical meteorology / Intertropical Convergence Zone / Low-pressure area / Coriolis effect / Atmosphere of Earth / Troposphere / Benoît Paul Émile Clapeyron / Atmospheric sciences / Meteorology / Atmospheric thermodynamics](https://www.pdfsearch.io/img/a514317f15d305d27a89608f3a5a8315.jpg) Date: 2014-12-10 12:58:09Atmospheric dynamics Atmosphere Tropical meteorology Intertropical Convergence Zone Low-pressure area Coriolis effect Atmosphere of Earth Troposphere Benoît Paul Émile Clapeyron Atmospheric sciences Meteorology Atmospheric thermodynamics | | 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 Add to Reading ListSource URL: web.gps.caltech.eduDownload Document from Source Website File Size: 1,44 MBShare Document on Facebook
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