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contributor authorSchär, Christoph
date accessioned2017-06-09T14:31:27Z
date available2017-06-09T14:31:27Z
date copyright1993/05/01
date issued1993
identifier issn0022-4928
identifier otherams-20916.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157197
description abstractThe conservation of potential vorticity Q can be expressed as ?(?Q/?t + ?·J = 0, where J denotes the total flux of potential vorticity. It is shown that J is related under statistically steady conditions to the Bernoulli function B by J = ?? ? ?B,where ? is the potential temperature. This relation is valid even in the nonhydrostatic limit and in the presence of arbitrary nonconservative forces (such as internal friction) and heating rates. In essence, it can be interpreted as a generalization of Bernoulli's theorem to the frictional and diabatic regime. The classical Bernoulli theorem?valid for inviscid adiabatic and steady flows?states that the intersections of surfaces of constant potential temperature and constant Bernoulli function yield streamlines. In the presence of frictional and diabatic effects, these intersections yield the flux lines along which potential vorticity is transported.
publisherAmerican Meteorological Society
titleA Generalization of Bernoulli's Theorem
typeJournal Paper
journal volume50
journal issue10
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1993)050<1437:AGOBT>2.0.CO;2
journal fristpage1437
journal lastpage1443
treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 010
contenttypeFulltext


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