A COMPARISON OF THE RESPONSE OF THE NORTH AMERICAN AND EUROPEAN SURFACE PRESSURE DISTRIBUTIONS TO LARGE GEOMAGNETIC DISTURBANCESSource: Journal of Meteorology:;1959:;volume( 016 ):;issue: 005::page 569Author:Shapiro, Ralph
DOI: 10.1175/1520-0469(1959)016<0569:ACOTRO>2.0.CO;2Publisher: American Meteorological Society
Abstract: The persistence of the three-day mean surface pressure distribution in a mid-latitude region centered on the Greenwich meridian is examined in connection with large increases in geomagnetic activity and is compared with an earlier study concerned with the same parameters over a different region. The reactions of certain individual features of the pressure distributions of the two regions are also investigated.
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| contributor author | Shapiro, Ralph | |
| date accessioned | 2017-06-09T14:12:13Z | |
| date available | 2017-06-09T14:12:13Z | |
| date copyright | 1959/10/01 | |
| date issued | 1959 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-14562.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4150137 | |
| description abstract | The persistence of the three-day mean surface pressure distribution in a mid-latitude region centered on the Greenwich meridian is examined in connection with large increases in geomagnetic activity and is compared with an earlier study concerned with the same parameters over a different region. The reactions of certain individual features of the pressure distributions of the two regions are also investigated. | |
| publisher | American Meteorological Society | |
| title | A COMPARISON OF THE RESPONSE OF THE NORTH AMERICAN AND EUROPEAN SURFACE PRESSURE DISTRIBUTIONS TO LARGE GEOMAGNETIC DISTURBANCES | |
| type | Journal Paper | |
| journal volume | 16 | |
| journal issue | 5 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1959)016<0569:ACOTRO>2.0.CO;2 | |
| journal fristpage | 569 | |
| journal lastpage | 572 | |
| tree | Journal of Meteorology:;1959:;volume( 016 ):;issue: 005 | |
| contenttype | Fulltext |