THE TEMPERATURE DEPENDENCE OF OZONE RADIATIONAL HEATING RATES IN THE VICINITY OF THE MESOPEAK

dc.contributor.author	Craig, Richard A.
dc.contributor.author	Ohring, George
dc.date.accessioned	2017-06-09T14:11:49Z
dc.date.available	2017-06-09T14:11:49Z
dc.date.copyright	1958/02/01
dc.date.issued	1958
dc.identifier.issn	0095-9634
dc.identifier.other	ams-14401.pdf
dc.identifier.uri	http://onlinelibrary.yabesh.ir/handle/yetl/4149959
dc.description.abstract	Radiational heating of the mesosphere results principally from absorption of ultraviolet radiation by ozone. For conditions of photochemical equilibrium, the amount of ozone present near the mesopeak depends critically on the temperature. Relatively high temperature results in less ozone and less heating. Calculations presented herein show that this effect has a strong stabilizing influence on the temperature values near the mesopeak.
dc.publisher	American Meteorological Society
dc.title	THE TEMPERATURE DEPENDENCE OF OZONE RADIATIONAL HEATING RATES IN THE VICINITY OF THE MESOPEAK
dc.type	Journal Paper
dc.journal.volume	15
dc.journal.issue	1
dc.journal.title	Journal of Meteorology
dc.identifier.doi	10.1175/1520-0469(1958)015<0059:TTDOOR>2.0.CO;2
dc.journal.fristpage	59
dc.journal.lastpage	62
dc.tree	Journal of Meteorology:;1958:;volume( 015 ):;issue: 001
dc.contenttype	Fulltext