The large-amplitude, low-zonal-index 700-mb. circulation
[l] was replaced in August by highindex flow (figs. 1 and 2). Much of this change was related to the development of a strong blocking High over Davis Strait. The positive height anomaly center with this ridge reflects an apparent retrogression from the positive center at 50 ' N., 30 ' W. i...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.395.1664 2023-05-15T16:00:12+02:00 The large-amplitude, low-zonal-index 700-mb. circulation James F. Andrews The Pennsylvania State University CiteSeerX Archives 1966 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.1664 http://docs.lib.noaa.gov/rescue/mwr/094/mwr-094-11-0669.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.1664 http://docs.lib.noaa.gov/rescue/mwr/094/mwr-094-11-0669.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://docs.lib.noaa.gov/rescue/mwr/094/mwr-094-11-0669.pdf text 1966 ftciteseerx 2016-01-08T02:26:18Z [l] was replaced in August by highindex flow (figs. 1 and 2). Much of this change was related to the development of a strong blocking High over Davis Strait. The positive height anomaly center with this ridge reflects an apparent retrogression from the positive center at 50 ' N., 30 ' W. in July. Heights at 700 mb. in mid-Atlantic fell as much as 500 ft. (fig. 3) as blocking became established at high latitudes over the Atlantic and North America. Fast, zonal flow then prevailed across the Atlantic in August as the westerlies were displaced slightly south of normal. The primary track of migratory cyclones, also farther south than normal, was almost coincident with the axis of negative 700-mb. height anomaly (fig. 2). Long waves over North America retrograded from Text Davis Strait Unknown |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
[l] was replaced in August by highindex flow (figs. 1 and 2). Much of this change was related to the development of a strong blocking High over Davis Strait. The positive height anomaly center with this ridge reflects an apparent retrogression from the positive center at 50 ' N., 30 ' W. in July. Heights at 700 mb. in mid-Atlantic fell as much as 500 ft. (fig. 3) as blocking became established at high latitudes over the Atlantic and North America. Fast, zonal flow then prevailed across the Atlantic in August as the westerlies were displaced slightly south of normal. The primary track of migratory cyclones, also farther south than normal, was almost coincident with the axis of negative 700-mb. height anomaly (fig. 2). Long waves over North America retrograded from |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
James F. Andrews |
spellingShingle |
James F. Andrews The large-amplitude, low-zonal-index 700-mb. circulation |
author_facet |
James F. Andrews |
author_sort |
James F. Andrews |
title |
The large-amplitude, low-zonal-index 700-mb. circulation |
title_short |
The large-amplitude, low-zonal-index 700-mb. circulation |
title_full |
The large-amplitude, low-zonal-index 700-mb. circulation |
title_fullStr |
The large-amplitude, low-zonal-index 700-mb. circulation |
title_full_unstemmed |
The large-amplitude, low-zonal-index 700-mb. circulation |
title_sort |
large-amplitude, low-zonal-index 700-mb. circulation |
publishDate |
1966 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.1664 http://docs.lib.noaa.gov/rescue/mwr/094/mwr-094-11-0669.pdf |
genre |
Davis Strait |
genre_facet |
Davis Strait |
op_source |
http://docs.lib.noaa.gov/rescue/mwr/094/mwr-094-11-0669.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.1664 http://docs.lib.noaa.gov/rescue/mwr/094/mwr-094-11-0669.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766396100463296512 |