Strong storms are regular features over the ocean west of Alaska. These systems often loiter, generating moderate to severe marine states which can exhibit persistence, maximizing damage and hazard potential. This analysis presents the wave states associated with selected storms over the Bering and Chukchi Seas. These include the damaging events of October 2004, September 2005, and November 2009, along with a strong event from September 2011 that exhibited north winds. For each event a brief synoptic overview is presented followed by consideration of the resultant wave state, including parameters such as wave steepness. Wave data come from NOAA’s WAVEWATCH III operational global ocean wave model, implemented locally on the Arctic Region Sup...
AbstractWe develop a conceptual model of the closely co-dependent Bering shelf, Bering Strait, and C...
Pacific Northwest coasts are exposed to coastal inundation as a result of storm surge and large wave...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95536/1/jgrc12221.pd
Within the period of the historical record there have been several occurrences of extensive damage f...
The North Pacific and Bering Sea regions represent loci of cyclogenesis and storm track activity. In...
The native Inupiaq community of Shaktoolik, in northwestern Alaska, is located on a low-lying barrie...
Wind‐driven changes in the path of warm Bering/Chukchi waters carried by the Alaska Coastal Current ...
AbstractThe sea state of the Beaufort and Chukchi seas is controlled by the wind forcing and the amo...
The northern coast of Alaska is experiencing significant climatic change enhancing hazards from redu...
Thesis (Master's)--University of Washington, 2019A relatively narrow (~85km) and shallow (~50m) Beri...
1. To validate the quality of available wind products through application of the WAM model Cycle 4.5...
Along the north slope of Alaska, shorefast ice protects the coast up to 9 months of the year and neg...
The sea state of the Beaufort and Chukchi seas is controlled by the wind forcing and the amount of i...
Thesis (Ph.D.) University of Alaska Fairbanks, 1976A bottom mounted surface wave gauge was operated ...
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of Ame...
AbstractWe develop a conceptual model of the closely co-dependent Bering shelf, Bering Strait, and C...
Pacific Northwest coasts are exposed to coastal inundation as a result of storm surge and large wave...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95536/1/jgrc12221.pd
Within the period of the historical record there have been several occurrences of extensive damage f...
The North Pacific and Bering Sea regions represent loci of cyclogenesis and storm track activity. In...
The native Inupiaq community of Shaktoolik, in northwestern Alaska, is located on a low-lying barrie...
Wind‐driven changes in the path of warm Bering/Chukchi waters carried by the Alaska Coastal Current ...
AbstractThe sea state of the Beaufort and Chukchi seas is controlled by the wind forcing and the amo...
The northern coast of Alaska is experiencing significant climatic change enhancing hazards from redu...
Thesis (Master's)--University of Washington, 2019A relatively narrow (~85km) and shallow (~50m) Beri...
1. To validate the quality of available wind products through application of the WAM model Cycle 4.5...
Along the north slope of Alaska, shorefast ice protects the coast up to 9 months of the year and neg...
The sea state of the Beaufort and Chukchi seas is controlled by the wind forcing and the amount of i...
Thesis (Ph.D.) University of Alaska Fairbanks, 1976A bottom mounted surface wave gauge was operated ...
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of Ame...
AbstractWe develop a conceptual model of the closely co-dependent Bering shelf, Bering Strait, and C...
Pacific Northwest coasts are exposed to coastal inundation as a result of storm surge and large wave...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95536/1/jgrc12221.pd