A 32-km Moist Primitive Equation Model Providing for Scale Interaction

dc.contributor.author	Kaplan, Michael L.
dc.contributor.author	Paine, Douglas A.
dc.date.accessioned	2017-06-09T14:16:48Z
dc.date.available	2017-06-09T14:16:48Z
dc.date.copyright	1973/03/01
dc.date.issued	1973
dc.identifier.issn	0022-4928
dc.identifier.other	ams-16318.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4152088
dc.description.abstract	A numerical model has been developed in an effort to simulate the interaction between quasi-geostrophic and mesoscale forcing. Initializations performed at 127 km with either a diagnostic omega equation or barotropic forecast are followed by a prediction with a moist nine-level primitive equation model at 32 km. Several integrations are performed utilizing both real and artificial data for the problem of the water-induced heat island in the cold season. The results of these integrations indicate important variations in both the patterns and intensity of development as a function of initialization.
dc.publisher	American Meteorological Society
dc.title	A 32-km Moist Primitive Equation Model Providing for Scale Interaction
dc.type	Journal Paper
dc.journal.volume	30
dc.journal.issue	2
dc.journal.title	Journal of the Atmospheric Sciences
dc.identifier.doi	10.1175/1520-0469(1973)030<0213:AKMPEM>2.0.CO;2
dc.journal.fristpage	213
dc.journal.lastpage	222
dc.tree	Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 002
dc.contenttype	Fulltext