Alaskan Arctic Coastal Processes and Morphology

A study of the temporal and spatial variability of the physical processes and environments of the Alaskan Arctic Coast was conducted over a 2- year period (May 1971 - June 1973). Micrometeorological studies demonstrated the difficulty of characterizing momentum transfer from air to ice by a single c...

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Main Authors: Wiseman, Jr , William J, Coleman, James M, Gregory, Anthony, Hsu, Shih-Ang, Short, Andrew D, Suhayda, J N, Waters, Jr , C D, Wright, L D
Other Authors: LOUISIANA STATE UNIV BATON ROUGE COASTAL STUDIES INST
Format: Text
Language:English
Published: 1973
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0766475
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0766475
id ftdtic:AD0766475
record_format openpolar
spelling ftdtic:AD0766475 2023-05-15T14:42:07+02:00 Alaskan Arctic Coastal Processes and Morphology Wiseman, Jr , William J Coleman, James M Gregory, Anthony Hsu, Shih-Ang Short, Andrew D Suhayda, J N Waters, Jr , C D Wright, L D LOUISIANA STATE UNIV BATON ROUGE COASTAL STUDIES INST 1973-07 text/html http://www.dtic.mil/docs/citations/AD0766475 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0766475 en eng http://www.dtic.mil/docs/citations/AD0766475 Approved for public release; distribution is unlimited. DTIC AND NTIS Physical and Dynamic Oceanography *ALASKA ARCTIC OCEAN BEACHES COASTAL REGIONS ENVIRONMENTS EROSION FREEZING INTERACTIONS MELTING MICROMETEOROLOGY OCEAN WAVES RIVERS SEA ICE SEDIMENTATION SNOW STORMS WIND AIR WATER INTERACTIONS COASTAL MORPHOLOGY Text 1973 ftdtic 2016-02-24T14:03:18Z A study of the temporal and spatial variability of the physical processes and environments of the Alaskan Arctic Coast was conducted over a 2- year period (May 1971 - June 1973). Micrometeorological studies demonstrated the difficulty of characterizing momentum transfer from air to ice by a single constant drag coefficient but indicated that such a coefficient may characterize air-sea momentum transfer in the nearshore waters. Summer wind-driven currents were far stronger and more variable than those during the winter season. They caused large meteorological tides and subsequent modification of the nearshore water mass characteristics. Statistically significant contrasts were noted between the morphology of the Chukchi and Beaufort coasts. The study demonstrated the dominance of storm-induced modification of the nearshore region and indicated that the arctic coastal environment cannot be adequately characterized from short-term studies conducted during moderate conditions. Sponsored in part by DARPA. Text Arctic Arctic Ocean Chukchi Sea ice Alaska Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
*ALASKA
ARCTIC OCEAN
BEACHES
COASTAL REGIONS
ENVIRONMENTS
EROSION
FREEZING
INTERACTIONS
MELTING
MICROMETEOROLOGY
OCEAN WAVES
RIVERS
SEA ICE
SEDIMENTATION
SNOW
STORMS
WIND
AIR WATER INTERACTIONS
COASTAL MORPHOLOGY
spellingShingle Physical and Dynamic Oceanography
*ALASKA
ARCTIC OCEAN
BEACHES
COASTAL REGIONS
ENVIRONMENTS
EROSION
FREEZING
INTERACTIONS
MELTING
MICROMETEOROLOGY
OCEAN WAVES
RIVERS
SEA ICE
SEDIMENTATION
SNOW
STORMS
WIND
AIR WATER INTERACTIONS
COASTAL MORPHOLOGY
Wiseman, Jr , William J
Coleman, James M
Gregory, Anthony
Hsu, Shih-Ang
Short, Andrew D
Suhayda, J N
Waters, Jr , C D
Wright, L D
Alaskan Arctic Coastal Processes and Morphology
topic_facet Physical and Dynamic Oceanography
*ALASKA
ARCTIC OCEAN
BEACHES
COASTAL REGIONS
ENVIRONMENTS
EROSION
FREEZING
INTERACTIONS
MELTING
MICROMETEOROLOGY
OCEAN WAVES
RIVERS
SEA ICE
SEDIMENTATION
SNOW
STORMS
WIND
AIR WATER INTERACTIONS
COASTAL MORPHOLOGY
description A study of the temporal and spatial variability of the physical processes and environments of the Alaskan Arctic Coast was conducted over a 2- year period (May 1971 - June 1973). Micrometeorological studies demonstrated the difficulty of characterizing momentum transfer from air to ice by a single constant drag coefficient but indicated that such a coefficient may characterize air-sea momentum transfer in the nearshore waters. Summer wind-driven currents were far stronger and more variable than those during the winter season. They caused large meteorological tides and subsequent modification of the nearshore water mass characteristics. Statistically significant contrasts were noted between the morphology of the Chukchi and Beaufort coasts. The study demonstrated the dominance of storm-induced modification of the nearshore region and indicated that the arctic coastal environment cannot be adequately characterized from short-term studies conducted during moderate conditions. Sponsored in part by DARPA.
author2 LOUISIANA STATE UNIV BATON ROUGE COASTAL STUDIES INST
format Text
author Wiseman, Jr , William J
Coleman, James M
Gregory, Anthony
Hsu, Shih-Ang
Short, Andrew D
Suhayda, J N
Waters, Jr , C D
Wright, L D
author_facet Wiseman, Jr , William J
Coleman, James M
Gregory, Anthony
Hsu, Shih-Ang
Short, Andrew D
Suhayda, J N
Waters, Jr , C D
Wright, L D
author_sort Wiseman, Jr , William J
title Alaskan Arctic Coastal Processes and Morphology
title_short Alaskan Arctic Coastal Processes and Morphology
title_full Alaskan Arctic Coastal Processes and Morphology
title_fullStr Alaskan Arctic Coastal Processes and Morphology
title_full_unstemmed Alaskan Arctic Coastal Processes and Morphology
title_sort alaskan arctic coastal processes and morphology
publishDate 1973
url http://www.dtic.mil/docs/citations/AD0766475
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0766475
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Chukchi
Sea ice
Alaska
genre_facet Arctic
Arctic Ocean
Chukchi
Sea ice
Alaska
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0766475
op_rights Approved for public release; distribution is unlimited.
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