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contributor authorForsythe, George E.
date accessioned2017-06-09T14:10:05Z
date available2017-06-09T14:10:05Z
date copyright1949/10/01
date issued1949
identifier issn0095-9634
identifier otherams-13708.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149188
description abstractThe pressure and density fields are assumed known exactly for all time, and the wind is to be forecast by obtaining the trajectory of each air particle from the equations of nonviscous motion in a plane. The importance of initial conditions is stressed. For sufficiently simple pressure and density fields the particle trajectories and hodographs may be obtained explicitly without approximation. The appropriate mathematical methods are reviewed. When the pressure force depends only on time, the solutions are compared with the Brunt?Douglas ?isallobaric-wind? formula. For one case of stationary circular isobars the exact solution is shown to consist of a superposition of so-called ?normal? and ?abnormal? solutions of the gradient wind equation. Explicit trajectories believed to be new are found for an air parcel in a certain high-pressure center whose horizontal pressure gradient is equal to or greater than that of the so-called maximum anticyclone. The general nonlinear case of circular isobars is discussed. Several numerical examples are included.
publisherAmerican Meteorological Society
titleEXACT PARTICLE TRAJECTORIES FOR NONVISCOUS FLOW IN A PLANE WITH A CONSTANT CORIOLIS PARAMETER
typeJournal Paper
journal volume6
journal issue5
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1949)006<0337:EPTFNF>2.0.CO;2
journal fristpage337
journal lastpage346
treeJournal of Meteorology:;1949:;volume( 006 ):;issue: 005
contenttypeFulltext


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