CEAREX: Hydrography, Acoustic Doppler Current Studies and Numerical Modeling of Eddies and their Interaction with the MIZ
The long-term goals are to understand how the marginal ice edge zone (MIZ) interacts with the open ocean in an oceanographic/meteorological/ biological sense. This includes understanding the processes and dynamics for the generation, dissipation and role of mesoscale eddies and chimneys in the MIZ (...
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ftdtic:ADA261536 2023-05-15T16:18:04+02:00 CEAREX: Hydrography, Acoustic Doppler Current Studies and Numerical Modeling of Eddies and their Interaction with the MIZ Niebauer, Henry J. ALASKA UNIV FAIRBANKS INST OF MARINE SCIENCE 1992-12-23 text/html http://www.dtic.mil/docs/citations/ADA261536 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA261536 en eng http://www.dtic.mil/docs/citations/ADA261536 Approved for public release; distribution is unlimited. DTIC AND NTIS Snow Ice and Permafrost *MARGINAL ICE ZONES MATHEMATICAL MODELS INTERACTIONS NAVAL RESEARCH OCEANS FRAM STRAIT CARBON DIOXIDE DEEP OCEANS GREENLAND SEA M12(MARGINAL ICE EDGE ZONES) EDDRES(OCEANOGRAPHY) Text 1992 ftdtic 2016-02-22T08:52:52Z The long-term goals are to understand how the marginal ice edge zone (MIZ) interacts with the open ocean in an oceanographic/meteorological/ biological sense. This includes understanding the processes and dynamics for the generation, dissipation and role of mesoscale eddies and chimneys in the MIZ (and in the open ocean after the ice has retreated or melted) in the Greenland Sea/Fram Strait. A further goal is to understand how these physical features interact with the biological and chemical oceanography causing enhancement of biological production in the MIZ and adjacent open ocean. All of this is aimed at understanding the physical and biological controls on the visible and acoustic environment of the MIZ. It is also aimed at understanding the effects of interannual variability and global change which result in variability in flux of carbon, through primary production, to the deep ocean possibly buffering CO2 in the atmosphere. Text Fram Strait Greenland Greenland Sea Ice permafrost Defense Technical Information Center: DTIC Technical Reports database Greenland |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost *MARGINAL ICE ZONES MATHEMATICAL MODELS INTERACTIONS NAVAL RESEARCH OCEANS FRAM STRAIT CARBON DIOXIDE DEEP OCEANS GREENLAND SEA M12(MARGINAL ICE EDGE ZONES) EDDRES(OCEANOGRAPHY) |
spellingShingle |
Snow Ice and Permafrost *MARGINAL ICE ZONES MATHEMATICAL MODELS INTERACTIONS NAVAL RESEARCH OCEANS FRAM STRAIT CARBON DIOXIDE DEEP OCEANS GREENLAND SEA M12(MARGINAL ICE EDGE ZONES) EDDRES(OCEANOGRAPHY) Niebauer, Henry J. CEAREX: Hydrography, Acoustic Doppler Current Studies and Numerical Modeling of Eddies and their Interaction with the MIZ |
topic_facet |
Snow Ice and Permafrost *MARGINAL ICE ZONES MATHEMATICAL MODELS INTERACTIONS NAVAL RESEARCH OCEANS FRAM STRAIT CARBON DIOXIDE DEEP OCEANS GREENLAND SEA M12(MARGINAL ICE EDGE ZONES) EDDRES(OCEANOGRAPHY) |
description |
The long-term goals are to understand how the marginal ice edge zone (MIZ) interacts with the open ocean in an oceanographic/meteorological/ biological sense. This includes understanding the processes and dynamics for the generation, dissipation and role of mesoscale eddies and chimneys in the MIZ (and in the open ocean after the ice has retreated or melted) in the Greenland Sea/Fram Strait. A further goal is to understand how these physical features interact with the biological and chemical oceanography causing enhancement of biological production in the MIZ and adjacent open ocean. All of this is aimed at understanding the physical and biological controls on the visible and acoustic environment of the MIZ. It is also aimed at understanding the effects of interannual variability and global change which result in variability in flux of carbon, through primary production, to the deep ocean possibly buffering CO2 in the atmosphere. |
author2 |
ALASKA UNIV FAIRBANKS INST OF MARINE SCIENCE |
format |
Text |
author |
Niebauer, Henry J. |
author_facet |
Niebauer, Henry J. |
author_sort |
Niebauer, Henry J. |
title |
CEAREX: Hydrography, Acoustic Doppler Current Studies and Numerical Modeling of Eddies and their Interaction with the MIZ |
title_short |
CEAREX: Hydrography, Acoustic Doppler Current Studies and Numerical Modeling of Eddies and their Interaction with the MIZ |
title_full |
CEAREX: Hydrography, Acoustic Doppler Current Studies and Numerical Modeling of Eddies and their Interaction with the MIZ |
title_fullStr |
CEAREX: Hydrography, Acoustic Doppler Current Studies and Numerical Modeling of Eddies and their Interaction with the MIZ |
title_full_unstemmed |
CEAREX: Hydrography, Acoustic Doppler Current Studies and Numerical Modeling of Eddies and their Interaction with the MIZ |
title_sort |
cearex: hydrography, acoustic doppler current studies and numerical modeling of eddies and their interaction with the miz |
publishDate |
1992 |
url |
http://www.dtic.mil/docs/citations/ADA261536 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA261536 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Fram Strait Greenland Greenland Sea Ice permafrost |
genre_facet |
Fram Strait Greenland Greenland Sea Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA261536 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766004154370621440 |