SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska

Alaska’s Prince William Sound (PWS) is a unique locale tending to have strong gap winds, especially in the winter season. To characterize and understand these strong surface winds, which have great impacts on the local marine and aviation activities, the surface wind retrieval from the Syntheti...

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Bibliographic Details
Main Authors: Karl Volz, Peter Q Olsson, Haibo Liu
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2008
Subjects:
SAR
Online Access:https://doaj.org/article/65a54f3f4ae84b81b0eb6402db869a7f
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spelling ftdoajarticles:oai:doaj.org/article:65a54f3f4ae84b81b0eb6402db869a7f 2023-05-15T16:22:36+02:00 SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska Karl Volz Peter Q Olsson Haibo Liu 2008-08-01T00:00:00Z https://doaj.org/article/65a54f3f4ae84b81b0eb6402db869a7f EN eng MDPI AG http://www.mdpi.com/1424-8220/8/8/4894/ https://doaj.org/toc/1424-8220 1424-8220 https://doaj.org/article/65a54f3f4ae84b81b0eb6402db869a7f Sensors, Vol 8, Iss 8, Pp 4894-4914 (2008) SAR model gap wind barrier Alaska Chemical technology TP1-1185 article 2008 ftdoajarticles 2022-12-30T20:03:11Z Alaska’s Prince William Sound (PWS) is a unique locale tending to have strong gap winds, especially in the winter season. To characterize and understand these strong surface winds, which have great impacts on the local marine and aviation activities, the surface wind retrieval from the Synthetic Aperture Radar data (SAR-wind) is combined with a numerical mesoscale model. Helped with the SAR-wind observations, the mesoscale model is used to study cases of strong winds and relatively weak winds to depict the nature of these winds, including the area of extent and possible causes of the wind regimes. The gap winds from the Wells Passage and the Valdez Arm are the most dominant gap winds in PWS. Though the Valdez Arm is north-south trending and Wells Passage is east-west oriented, gap winds often develop simultaneously in these two places when a low pressure system is present in the Northern Gulf of Alaska. These two gap winds often converge at the center of PWS and extend further out of the Sound through the Hinchinbrook Entrance. The pressure gradients imposed over these areas are the main driving forces for these gap winds. Additionally, the drainage from the upper stream glaciers and the blocking effect of the banks of the Valdez Arm probably play an important role in enhancing the gap wind. Article in Journal/Newspaper glaciers Alaska Directory of Open Access Journals: DOAJ Articles Gulf of Alaska
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic SAR
model
gap wind
barrier
Alaska
Chemical technology
TP1-1185
spellingShingle SAR
model
gap wind
barrier
Alaska
Chemical technology
TP1-1185
Karl Volz
Peter Q Olsson
Haibo Liu
SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska
topic_facet SAR
model
gap wind
barrier
Alaska
Chemical technology
TP1-1185
description Alaska’s Prince William Sound (PWS) is a unique locale tending to have strong gap winds, especially in the winter season. To characterize and understand these strong surface winds, which have great impacts on the local marine and aviation activities, the surface wind retrieval from the Synthetic Aperture Radar data (SAR-wind) is combined with a numerical mesoscale model. Helped with the SAR-wind observations, the mesoscale model is used to study cases of strong winds and relatively weak winds to depict the nature of these winds, including the area of extent and possible causes of the wind regimes. The gap winds from the Wells Passage and the Valdez Arm are the most dominant gap winds in PWS. Though the Valdez Arm is north-south trending and Wells Passage is east-west oriented, gap winds often develop simultaneously in these two places when a low pressure system is present in the Northern Gulf of Alaska. These two gap winds often converge at the center of PWS and extend further out of the Sound through the Hinchinbrook Entrance. The pressure gradients imposed over these areas are the main driving forces for these gap winds. Additionally, the drainage from the upper stream glaciers and the blocking effect of the banks of the Valdez Arm probably play an important role in enhancing the gap wind.
format Article in Journal/Newspaper
author Karl Volz
Peter Q Olsson
Haibo Liu
author_facet Karl Volz
Peter Q Olsson
Haibo Liu
author_sort Karl Volz
title SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska
title_short SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska
title_full SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska
title_fullStr SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska
title_full_unstemmed SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska
title_sort sar observation and modeling of gap winds in the prince william sound of alaska
publisher MDPI AG
publishDate 2008
url https://doaj.org/article/65a54f3f4ae84b81b0eb6402db869a7f
geographic Gulf of Alaska
geographic_facet Gulf of Alaska
genre glaciers
Alaska
genre_facet glaciers
Alaska
op_source Sensors, Vol 8, Iss 8, Pp 4894-4914 (2008)
op_relation http://www.mdpi.com/1424-8220/8/8/4894/
https://doaj.org/toc/1424-8220
1424-8220
https://doaj.org/article/65a54f3f4ae84b81b0eb6402db869a7f
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