Mesoscale dynamics and orographic channeling of low-level flow through Nares Strait

model estimates of low-level winds and surface wind stress through Nares Strait, be-tween Ellesmere Island and Greenland, during two years from August 2003 through July 2005. Analysis of the model results during these two periods also suggest that the intense, low-level, along-strait winds are stron...

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Bibliographic Details
Main Authors: R. M. Samelson, P. Barbour
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2006
Subjects:
Ellesmere Island
Greenland
Nares
Nares strait
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.7035
http://www.udel.edu/CATS/reports/OSU2006/NS_Climat_v0.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.531.7035
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.531.7035 2023-05-15T16:05:55+02:00 Mesoscale dynamics and orographic channeling of low-level flow through Nares Strait R. M. Samelson P. Barbour The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.7035 http://www.udel.edu/CATS/reports/OSU2006/NS_Climat_v0.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.7035 http://www.udel.edu/CATS/reports/OSU2006/NS_Climat_v0.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.udel.edu/CATS/reports/OSU2006/NS_Climat_v0.pdf text 2006 ftciteseerx 2016-01-08T10:38:25Z model estimates of low-level winds and surface wind stress through Nares Strait, be-tween Ellesmere Island and Greenland, during two years from August 2003 through July 2005. Analysis of the model results during these two periods also suggest that the intense, low-level, along-strait winds are strongly ageostrophic, and may be usefully estimated from pressure differences along the Strait. 1 Text Ellesmere Island Greenland Nares strait Unknown Ellesmere Island Greenland Nares ENVELOPE(158.167,158.167,-81.450,-81.450)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description model estimates of low-level winds and surface wind stress through Nares Strait, be-tween Ellesmere Island and Greenland, during two years from August 2003 through July 2005. Analysis of the model results during these two periods also suggest that the intense, low-level, along-strait winds are strongly ageostrophic, and may be usefully estimated from pressure differences along the Strait. 1
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author R. M. Samelson
P. Barbour
spellingShingle R. M. Samelson
P. Barbour
Mesoscale dynamics and orographic channeling of low-level flow through Nares Strait
author_facet R. M. Samelson
P. Barbour
author_sort R. M. Samelson
title Mesoscale dynamics and orographic channeling of low-level flow through Nares Strait
title_short Mesoscale dynamics and orographic channeling of low-level flow through Nares Strait
title_full Mesoscale dynamics and orographic channeling of low-level flow through Nares Strait
title_fullStr Mesoscale dynamics and orographic channeling of low-level flow through Nares Strait
title_full_unstemmed Mesoscale dynamics and orographic channeling of low-level flow through Nares Strait
title_sort mesoscale dynamics and orographic channeling of low-level flow through nares strait
publishDate 2006
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.7035
http://www.udel.edu/CATS/reports/OSU2006/NS_Climat_v0.pdf
long_lat ENVELOPE(158.167,158.167,-81.450,-81.450)
geographic Ellesmere Island
Greenland
Nares
geographic_facet Ellesmere Island
Greenland
Nares
genre Ellesmere Island
Greenland
Nares strait
genre_facet Ellesmere Island
Greenland
Nares strait
op_source http://www.udel.edu/CATS/reports/OSU2006/NS_Climat_v0.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.7035
http://www.udel.edu/CATS/reports/OSU2006/NS_Climat_v0.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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