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
Language:English
Published: MDPI AG 2008-08-01
Series:Sensors
Subjects:
SAR
Online Access:http://www.mdpi.com/1424-8220/8/8/4894/
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spelling doaj-65a54f3f4ae84b81b0eb6402db869a7f2020-11-24T21:33:00ZengMDPI AGSensors1424-82202008-08-018848944914SAR Observation and Modeling of Gap Winds in the Prince William Sound of AlaskaKarl VolzPeter Q OlssonHaibo LiuAlaska’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.http://www.mdpi.com/1424-8220/8/8/4894/SARmodelgap windbarrierAlaska.
collection DOAJ
language English
format Article
sources DOAJ
author Karl Volz
Peter Q Olsson
Haibo Liu
spellingShingle Karl Volz
Peter Q Olsson
Haibo Liu
SAR Observation and Modeling of Gap Winds in the Prince William Sound of Alaska
Sensors
SAR
model
gap wind
barrier
Alaska.
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
series Sensors
issn 1424-8220
publishDate 2008-08-01
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.
topic SAR
model
gap wind
barrier
Alaska.
url http://www.mdpi.com/1424-8220/8/8/4894/
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AT peterqolsson sarobservationandmodelingofgapwindsintheprincewilliamsoundofalaska
AT haiboliu sarobservationandmodelingofgapwindsintheprincewilliamsoundofalaska
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