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contributor authorStan, Cristiana
contributor authorRandall, David A.
date accessioned2017-06-09T16:53:24Z
date available2017-06-09T16:53:24Z
date copyright2007/02/01
date issued2007
identifier issn0022-4928
identifier otherams-76023.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218425
description abstractThe dynamical equations of atmospheric flow are written using potential vorticity as the meridional coordinate and potential temperature as the vertical coordinate. Within this system, the atmosphere is divided into undulating tubes bounded by isentropic and constant potential vorticity surfaces, and, under adiabatic and frictionless conditions, the air moves through the tubes without penetrating through the walls.
publisherAmerican Meteorological Society
titlePotential Vorticity as Meridional Coordinate
typeJournal Paper
journal volume64
journal issue2
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/JAS3839.1
journal fristpage621
journal lastpage633
treeJournal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 002
contenttypeFulltext


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