A BAROCLINIC MODEL ATMOSPHERE SUITABLE FOR NUMERICAL INTEGRATION

dc.contributor.author	Sawyer, J. S.
dc.contributor.author	Bushby, F. H.
dc.date.accessioned	2017-06-09T14:10:41Z
dc.date.available	2017-06-09T14:10:41Z
dc.date.copyright	1953/02/01
dc.date.issued	1953
dc.identifier.issn	0095-9634
dc.identifier.other	ams-13963.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4149471
dc.description.abstract	Subject to various approximations, a system of three simultaneous partial differential equations is derived to predict the height of a contour surface, the thickness of the layer from 1000 mb to that surface, and the field of vertical velocity averaged throughout a vertical column. The equations are in a form suitable for numerical integration, and a brief outline of a method of solution is given.
dc.publisher	American Meteorological Society
dc.title	A BAROCLINIC MODEL ATMOSPHERE SUITABLE FOR NUMERICAL INTEGRATION
dc.type	Journal Paper
dc.journal.volume	10
dc.journal.issue	1
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1953)010<0054:ABMASF>2.0.CO;2
dc.journal.fristpage	54
dc.journal.lastpage	59
dc.tree	Journal of Meteorology:;1953:;volume( 010 ):;issue: 001
dc.contenttype	Fulltext