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dc.contributor.authorPressman, Jerome
dc.date.accessioned2017-06-09T14:11:08Z
dc.date.available2017-06-09T14:11:08Z
dc.date.copyright1955/02/01
dc.date.issued1955
dc.identifier.issn0095-9634
dc.identifier.otherams-14139.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149667
dc.description.abstractA calculation is made of seasonal and latitudinal temperature changes in the ozonosphere which would be caused solely by the absorption by ozone of solar radiation in the Huggins, Hartley and Chappius regions. A constant density of the atmosphere with season and latitude is assumed. Strong seasonal and latitudinal temperature changes are noted, with maximum increases over the poles during their respective summers.
dc.publisherAmerican Meteorological Society
dc.titleSEASONAL AND LATITUDINAL TEMPERATURE CHANGES IN THE OZONOSPHERE
dc.typeJournal Paper
dc.journal.volume12
dc.journal.issue1
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1955)012<0087:SALTCI>2.0.CO;2
dc.journal.fristpage87
dc.journal.lastpage89
dc.treeJournal of Meteorology:;1955:;volume( 012 ):;issue: 001
dc.contenttypeFulltext


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