Microstructure Casts during AIWEX (Arctic Internal Wave Experiment). A Summary
The Arctic Internal Wave Experience (AIWEX) was designed to study the internal wave and microstructure fields in in the Beaufort Sea in the early spring. A major goal of the experiment was to verify the hypothesis that the internal wave and microstructure fields beneath the ice are far less energeti...
Main Authors: | , , |
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Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1985
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Online Access: | http://www.dtic.mil/docs/citations/ADA181764 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA181764 |
Summary: | The Arctic Internal Wave Experience (AIWEX) was designed to study the internal wave and microstructure fields in in the Beaufort Sea in the early spring. A major goal of the experiment was to verify the hypothesis that the internal wave and microstructure fields beneath the ice are far less energetic than in temperate oceans. Major goals of the microstructure measurements were: to characterize the double-diffusive staircase region in the depth range 300-450m; to estimate the heat flux from the deep Atlantic water into shallower depth zones; and to assess the influence of mesoscale and submesoscale eddies on turbulence beneath the ice. Keywords: Underice internal waves; Spring season; Sea water eddies; Bathythermograph data; Electrical conductivity; Temperature/Salinity data; Staircase temperature profiles. |
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