| contributor author | DeLuisi, John J. | |
| contributor author | Furukawa, Paul M. | |
| date accessioned | 2017-06-09T14:15:34Z | |
| date available | 2017-06-09T14:15:34Z | |
| date copyright | 1970/09/01 | |
| date issued | 1970 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-15852.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4151570 | |
| description abstract | It is pointed out that the anomalous seasonal variation in the worldwide ozone concentration above 40 km deduced from Umkehr measurements is opposite to the seasonal variation in atmospheric turbidity. The maximum and minimum seasonal variation in turbidity is used to estimate a haze correction to an Umkehr observation. From a comparison of ozone concentration deduced from corrected and uncorrected Umkehrs it is noted that 1) increased turbidity reduces the ozone concentration at 45 km, and 2) the maximum seasonal change in turbidity can nearly, if not entirely, account for the maximum seasonal change (about 2 ?mb) in ozone concentration at 45 km. | |
| publisher | American Meteorological Society | |
| title | An Explanation for the Worldwide Anomaly in the Concentration of Ozone Above 40 km | |
| type | Journal Paper | |
| journal volume | 27 | |
| journal issue | 6 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1970)027<0968:AEFTWA>2.0.CO;2 | |
| journal fristpage | 968 | |
| journal lastpage | 970 | |
| tree | Journal of the Atmospheric Sciences:;1970:;Volume( 027 ):;issue: 006 | |
| contenttype | Fulltext | |