| contributor author | Boville, B. W. | |
| date accessioned | 2017-06-09T14:12:21Z | |
| date available | 2017-06-09T14:12:21Z | |
| date copyright | 1960/06/01 | |
| date issued | 1960 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-14627.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4150209 | |
| description abstract | The dominant feature of the 1958?59 polar-night circulation was the intense warm anticyclone which developed over the Aleutian-Alaskan area in October. The anticyclone persisted throughout the winter acting as an anchor ridge for the strong baroclinic waves in the polar-night stream. The character of the middle stratospheric domain and some features of the baroclinic waves are presented. The October anticyclogenesis which occurred with only moderate stratospheric baroclinity is related to tropospheric cyclogenesis by synoptic techniques and Fourier analysis. | |
| publisher | American Meteorological Society | |
| title | THE ALEUTIAN STRATOSPHERIC ANTICYCLONE | |
| type | Journal Paper | |
| journal volume | 17 | |
| journal issue | 3 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1960)017<0329:TASA>2.0.CO;2 | |
| journal fristpage | 329 | |
| journal lastpage | 336 | |
| tree | Journal of Meteorology:;1960:;volume( 017 ):;issue: 003 | |
| contenttype | Fulltext | |
