In meteorology, p _ 1 and p _ 2 are isobaric surfaces.
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In other words, it is a flow in which isobaric surfaces are isopycnic surfaces and vice versa.
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The temperature, humidity, and wind on aeroclimatic maps may apply either to standard altitudes or to the main isobaric surfaces.
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Such isobaric surfaces will also be isothermal surfaces, hence ( from the thermal wind equation ) the geostrophic wind will not vary with depth.
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In meteorology, a "'barotropic atmosphere "'is one that for which the density of the air depends only on pressure, as a result isobaric surfaces ( constant-pressure surfaces ) are also constant-density surfaces.
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The pressure field in free atmosphere is represented either by maps of the distribution of pressure at different standard altitudes for example, at every kilometer above sea level or by maps of baric topography on which altitudes ( more precisely geopotentials ) of the main isobaric surfaces ( for example, 900, 800, and 700 millibars ) counted off from sea level are plotted.
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