FRONTAL PASSAGES OVER THE NORTH ATLANTIC OCEAN
Graphical and tnbul;w tl;tt,:r on the freqwucy of frontal ~msnges at Ocean Station Vessels on the North Atlantic are compiled from historical wexther tl~aps for the years 1945-57. The stabilizing influence of the Gulf Stream is shown by the ra1)id modificatiorl of air temperature at all stations and...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.395.1552 2023-05-15T17:28:30+02:00 FRONTAL PASSAGES OVER THE NORTH ATLANTIC OCEAN Georgia C. Whiting The Pennsylvania State University CiteSeerX Archives 1959 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.1552 http://docs.lib.noaa.gov/rescue/mwr/087/mwr-087-11-0409.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.1552 http://docs.lib.noaa.gov/rescue/mwr/087/mwr-087-11-0409.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://docs.lib.noaa.gov/rescue/mwr/087/mwr-087-11-0409.pdf text 1959 ftciteseerx 2016-01-08T02:26:18Z Graphical and tnbul;w tl;tt,:r on the freqwucy of frontal ~msnges at Ocean Station Vessels on the North Atlantic are compiled from historical wexther tl~aps for the years 1945-57. The stabilizing influence of the Gulf Stream is shown by the ra1)id modificatiorl of air temperature at all stations and by the rapitl transition of frontal systems. The greatest freqnency of fronts is found at the line of initial contact of cooler air with that associated with the Gulf Stream in the westernulost region of the ocean. The value of the historical sea level synoptic wetither III~I~R as a (lata source for the climatological study of atmospheric luotion systems is euiplwsized. 1. Text North Atlantic Unknown |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Graphical and tnbul;w tl;tt,:r on the freqwucy of frontal ~msnges at Ocean Station Vessels on the North Atlantic are compiled from historical wexther tl~aps for the years 1945-57. The stabilizing influence of the Gulf Stream is shown by the ra1)id modificatiorl of air temperature at all stations and by the rapitl transition of frontal systems. The greatest freqnency of fronts is found at the line of initial contact of cooler air with that associated with the Gulf Stream in the westernulost region of the ocean. The value of the historical sea level synoptic wetither III~I~R as a (lata source for the climatological study of atmospheric luotion systems is euiplwsized. 1. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Georgia C. Whiting |
spellingShingle |
Georgia C. Whiting FRONTAL PASSAGES OVER THE NORTH ATLANTIC OCEAN |
author_facet |
Georgia C. Whiting |
author_sort |
Georgia C. Whiting |
title |
FRONTAL PASSAGES OVER THE NORTH ATLANTIC OCEAN |
title_short |
FRONTAL PASSAGES OVER THE NORTH ATLANTIC OCEAN |
title_full |
FRONTAL PASSAGES OVER THE NORTH ATLANTIC OCEAN |
title_fullStr |
FRONTAL PASSAGES OVER THE NORTH ATLANTIC OCEAN |
title_full_unstemmed |
FRONTAL PASSAGES OVER THE NORTH ATLANTIC OCEAN |
title_sort |
frontal passages over the north atlantic ocean |
publishDate |
1959 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.1552 http://docs.lib.noaa.gov/rescue/mwr/087/mwr-087-11-0409.pdf |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://docs.lib.noaa.gov/rescue/mwr/087/mwr-087-11-0409.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.395.1552 http://docs.lib.noaa.gov/rescue/mwr/087/mwr-087-11-0409.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766121211754971136 |