Spatial Variability of Total Ozone at High Latitudes in WinterSource: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 004::page 695Author:Kurzeja, Robert J.
DOI: 10.1175/1520-0469(1984)041<0695:SVOTOA>2.0.CO;2Publisher: American Meteorological Society
Abstract: The spatial variability of total ozone at high latitudes in winter is explained by the vertical structure of planetary-scale waves. The location of the maximum in total ozone is governed by the phase shift with height of the waves, while the amplitude of the maximum depends on the phase and also on the vertical and horizontal mean-zonal ozone gradients.
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| contributor author | Kurzeja, Robert J. | |
| date accessioned | 2017-06-09T14:24:36Z | |
| date available | 2017-06-09T14:24:36Z | |
| date copyright | 1984/02/01 | |
| date issued | 1984 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-18763.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4154804 | |
| description abstract | The spatial variability of total ozone at high latitudes in winter is explained by the vertical structure of planetary-scale waves. The location of the maximum in total ozone is governed by the phase shift with height of the waves, while the amplitude of the maximum depends on the phase and also on the vertical and horizontal mean-zonal ozone gradients. | |
| publisher | American Meteorological Society | |
| title | Spatial Variability of Total Ozone at High Latitudes in Winter | |
| type | Journal Paper | |
| journal volume | 41 | |
| journal issue | 4 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1984)041<0695:SVOTOA>2.0.CO;2 | |
| journal fristpage | 695 | |
| journal lastpage | 697 | |
| tree | Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 004 | |
| contenttype | Fulltext |