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contributor authorDonahue, T. M.
contributor authorGuenther, B.
contributor authorBlamont, J. E.
date accessioned2017-06-09T14:16:36Z
date available2017-06-09T14:16:36Z
date copyright1972/09/01
date issued1972
identifier issn0022-4928
identifier otherams-16245.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152007
description abstractObservations with a horizon scanning airglow photometer on OGO-6 have revealed the presence of a dense scattering layer near 80 km over the geographic pole during the local summer. The layer is detected on all satellite passes above 80° latitude beginning 15 days before the solstice. The optical depth of the layer increases by more than a factor of 50 between 70° and 85°. It is suggested that noctilucent clouds are weak sporadic manifestations of these persistent polar layers.
publisherAmerican Meteorological Society
titleNoctilucent Clouds in Daytime: Circumpolar Particulate Layers Near the Summer Mesopause
typeJournal Paper
journal volume29
journal issue6
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1972)029<1205:NCIDCP>2.0.CO;2
journal fristpage1205
journal lastpage1209
treeJournal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 006
contenttypeFulltext


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