Small and Mesoscale Processes in the Marginal Ice Zone Experiment.

The primary objective of this research program was to understand the spatial and temporal behavior of the finestructure in the upper ocean of the marginal ice zone and, in particular, to determine the role that internal waves play in determining the behavior of that finestructure. A secondary object...

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Bibliographic Details
Main Author: Foster, Theodore D
Other Authors: CALIFORNIA UNIV SANTA BARBARA MARINE SCIENCE INST
Format: Text
Language:English
Published: 1987
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA193143
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA193143
id ftdtic:ADA193143
record_format openpolar
spelling ftdtic:ADA193143 2023-05-15T16:37:09+02:00 Small and Mesoscale Processes in the Marginal Ice Zone Experiment. Foster, Theodore D CALIFORNIA UNIV SANTA BARBARA MARINE SCIENCE INST 1987-12-31 text/html http://www.dtic.mil/docs/citations/ADA193143 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA193143 en eng http://www.dtic.mil/docs/citations/ADA193143 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost *ICE *INTERNAL WAVES CALIBRATION ENERGY LEVELS HYDROGRAPHY INTRUSION OCEANS OPEN WATER PROFILES SALINITY SPECTRA TEMPERATURE OCEANOGRAPHIC DATA SEA WATER ELECTRICAL CONDUCTIVITY DENSITY Marginal ice zones. Text 1987 ftdtic 2016-02-19T11:08:47Z The primary objective of this research program was to understand the spatial and temporal behavior of the finestructure in the upper ocean of the marginal ice zone and, in particular, to determine the role that internal waves play in determining the behavior of that finestructure. A secondary objective was to provide high quality temperature and salinity profiles from the surface to the bottom in order to supplement the general hydrography of the region and to provide calibration data for other investigators. Analysis of the CTD times series data revealed that internal wave energy levels in the marginal ice zone are only slightly lower than those in the open ocean. We also showed that in the marginal ice zone intrusions make temperature spectra an invalid method for determining internal wave activity. Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ICE
*INTERNAL WAVES
CALIBRATION
ENERGY LEVELS
HYDROGRAPHY
INTRUSION
OCEANS
OPEN WATER
PROFILES
SALINITY
SPECTRA
TEMPERATURE
OCEANOGRAPHIC DATA
SEA WATER
ELECTRICAL CONDUCTIVITY
DENSITY
Marginal ice zones.
spellingShingle Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ICE
*INTERNAL WAVES
CALIBRATION
ENERGY LEVELS
HYDROGRAPHY
INTRUSION
OCEANS
OPEN WATER
PROFILES
SALINITY
SPECTRA
TEMPERATURE
OCEANOGRAPHIC DATA
SEA WATER
ELECTRICAL CONDUCTIVITY
DENSITY
Marginal ice zones.
Foster, Theodore D
Small and Mesoscale Processes in the Marginal Ice Zone Experiment.
topic_facet Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ICE
*INTERNAL WAVES
CALIBRATION
ENERGY LEVELS
HYDROGRAPHY
INTRUSION
OCEANS
OPEN WATER
PROFILES
SALINITY
SPECTRA
TEMPERATURE
OCEANOGRAPHIC DATA
SEA WATER
ELECTRICAL CONDUCTIVITY
DENSITY
Marginal ice zones.
description The primary objective of this research program was to understand the spatial and temporal behavior of the finestructure in the upper ocean of the marginal ice zone and, in particular, to determine the role that internal waves play in determining the behavior of that finestructure. A secondary objective was to provide high quality temperature and salinity profiles from the surface to the bottom in order to supplement the general hydrography of the region and to provide calibration data for other investigators. Analysis of the CTD times series data revealed that internal wave energy levels in the marginal ice zone are only slightly lower than those in the open ocean. We also showed that in the marginal ice zone intrusions make temperature spectra an invalid method for determining internal wave activity.
author2 CALIFORNIA UNIV SANTA BARBARA MARINE SCIENCE INST
format Text
author Foster, Theodore D
author_facet Foster, Theodore D
author_sort Foster, Theodore D
title Small and Mesoscale Processes in the Marginal Ice Zone Experiment.
title_short Small and Mesoscale Processes in the Marginal Ice Zone Experiment.
title_full Small and Mesoscale Processes in the Marginal Ice Zone Experiment.
title_fullStr Small and Mesoscale Processes in the Marginal Ice Zone Experiment.
title_full_unstemmed Small and Mesoscale Processes in the Marginal Ice Zone Experiment.
title_sort small and mesoscale processes in the marginal ice zone experiment.
publishDate 1987
url http://www.dtic.mil/docs/citations/ADA193143
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA193143
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA193143
op_rights APPROVED FOR PUBLIC RELEASE
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