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contributor authorBannon, Peter R.
contributor authorBishop, Craig H.
contributor authorKerr, James B.
date accessioned2017-06-09T14:42:01Z
date available2017-06-09T14:42:01Z
date copyright1997/11/01
date issued1997
identifier issn0003-0007
identifier otherams-24770.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161479
description abstractThe common statement that the surface pressure in a hydrostatic atmosphere is equal to the weight per unit area of the air aloft is shown to be true only for a Cartesian world. Here the unit area is the surface area of the base of the atmospheric column. For either a cylindrical or a spherical planet the surface pressure is always less than the weight per unit area of the overlying atmosphere. In these curved geometries, lateral pressure forces help support an individual column, thereby reducing the load carried by the surface pressure at the column's base. It is estimated that the surface pressure is a factor of 0.25% less than the weight per unit area of a resting atmosphere similar to that on Earth.
publisherAmerican Meteorological Society
titleDoes the Surface Pressure Equal the Weight per Unit Area of a Hydrostatic Atmosphere?
typeJournal Paper
journal volume78
journal issue11
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/1520-0477(1997)078<2637:DTSPET>2.0.CO;2
journal fristpage2637
journal lastpage2642
treeBulletin of the American Meteorological Society:;1997:;volume( 078 ):;issue: 011
contenttypeFulltext


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