THE WEATHER AND CIRCULATION OF APRIL 1952'
at both 700 mb. (fig. 1) and sea level (Chart XI). At both levels a deep mean trough extended from the Alaskan Arctic to the southeast Pacifk, with greatest negative anomalies centered in the Gulf of Alaska. The low latitude trough observed just south of California may be considered as an eastward e...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.394.6787 2023-05-15T15:02:42+02:00 THE WEATHER AND CIRCULATION OF APRIL 1952' Major Donald E. Martin The Pennsylvania State University CiteSeerX Archives 1952 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.6787 http://docs.lib.noaa.gov/rescue/mwr/080/mwr-080-04-0070.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.6787 http://docs.lib.noaa.gov/rescue/mwr/080/mwr-080-04-0070.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://docs.lib.noaa.gov/rescue/mwr/080/mwr-080-04-0070.pdf text 1952 ftciteseerx 2016-01-08T02:25:03Z at both 700 mb. (fig. 1) and sea level (Chart XI). At both levels a deep mean trough extended from the Alaskan Arctic to the southeast Pacifk, with greatest negative anomalies centered in the Gulf of Alaska. The low latitude trough observed just south of California may be considered as an eastward extension of the basic trough in the Gulf of Alaska. Thus, this trough tilted strongly from northwest to southeast. This was associated with a splitting of the westerlies and a southward transport of 1 See charts I-XV following page 76 for analyzed climatological data for the month. westerly momentum throughout the eastern Pacific. In eastern North America, on the other hand, the northern and southern streams of westerlies converged into a mean trough with strong tilt from northeast to southwest and extending from Florida to Iceland. The wave length Text Arctic Iceland Alaska Unknown Arctic Gulf of Alaska Pacific |
institution |
Open Polar |
collection |
Unknown |
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ftciteseerx |
language |
English |
description |
at both 700 mb. (fig. 1) and sea level (Chart XI). At both levels a deep mean trough extended from the Alaskan Arctic to the southeast Pacifk, with greatest negative anomalies centered in the Gulf of Alaska. The low latitude trough observed just south of California may be considered as an eastward extension of the basic trough in the Gulf of Alaska. Thus, this trough tilted strongly from northwest to southeast. This was associated with a splitting of the westerlies and a southward transport of 1 See charts I-XV following page 76 for analyzed climatological data for the month. westerly momentum throughout the eastern Pacific. In eastern North America, on the other hand, the northern and southern streams of westerlies converged into a mean trough with strong tilt from northeast to southwest and extending from Florida to Iceland. The wave length |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Major Donald E. Martin |
spellingShingle |
Major Donald E. Martin THE WEATHER AND CIRCULATION OF APRIL 1952' |
author_facet |
Major Donald E. Martin |
author_sort |
Major Donald |
title |
THE WEATHER AND CIRCULATION OF APRIL 1952' |
title_short |
THE WEATHER AND CIRCULATION OF APRIL 1952' |
title_full |
THE WEATHER AND CIRCULATION OF APRIL 1952' |
title_fullStr |
THE WEATHER AND CIRCULATION OF APRIL 1952' |
title_full_unstemmed |
THE WEATHER AND CIRCULATION OF APRIL 1952' |
title_sort |
weather and circulation of april 1952' |
publishDate |
1952 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.6787 http://docs.lib.noaa.gov/rescue/mwr/080/mwr-080-04-0070.pdf |
geographic |
Arctic Gulf of Alaska Pacific |
geographic_facet |
Arctic Gulf of Alaska Pacific |
genre |
Arctic Iceland Alaska |
genre_facet |
Arctic Iceland Alaska |
op_source |
http://docs.lib.noaa.gov/rescue/mwr/080/mwr-080-04-0070.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.394.6787 http://docs.lib.noaa.gov/rescue/mwr/080/mwr-080-04-0070.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766334617714950144 |