| contributor author | Donahue, T. M. | |
| contributor author | Guenther, B. | |
| contributor author | Blamont, J. E. | |
| date accessioned | 2017-06-09T14:16:36Z | |
| date available | 2017-06-09T14:16:36Z | |
| date copyright | 1972/09/01 | |
| date issued | 1972 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-16245.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4152007 | |
| description abstract | Observations 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. | |
| publisher | American Meteorological Society | |
| title | Noctilucent Clouds in Daytime: Circumpolar Particulate Layers Near the Summer Mesopause | |
| type | Journal Paper | |
| journal volume | 29 | |
| journal issue | 6 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1972)029<1205:NCIDCP>2.0.CO;2 | |
| journal fristpage | 1205 | |
| journal lastpage | 1209 | |
| tree | Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 006 | |
| contenttype | Fulltext | |