Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin

Our overall goal is to develop a quantitative understanding of processes that collectively make up the ice-albedo feedback mechanism. This mechanism is generally believed to be a key factor in amplifying natural variations within the earth s climate system. To achieve this understanding, we need to...

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Main Authors: Maykut, Gary A, Grenfell, Thomas C
Other Authors: WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES
Format: Text
Language:English
Published: 2001
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA625918
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA625918
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spelling ftdtic:ADA625918 2023-05-15T13:10:28+02:00 Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin Maykut, Gary A Grenfell, Thomas C WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES 2001-09-30 text/html http://www.dtic.mil/docs/citations/ADA625918 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA625918 en eng http://www.dtic.mil/docs/citations/ADA625918 Approved for public release; distribution is unlimited. DTIC Atmospheric Physics Physical and Dynamic Oceanography Snow Ice and Permafrost Optics *ALBEDO *OCEAN BASINS *PACK ICE ARCTIC OCEAN CLIMATE DISTRIBUTION FEEDBACK HEAT BALANCE PHYSICAL PROPERTIES RADIATION SHORT WAVELENGTHS *ICE-ALBEDO FEEDBACK SHORTWAVE RADIATION Text 2001 ftdtic 2016-02-24T19:42:05Z Our overall goal is to develop a quantitative understanding of processes that collectively make up the ice-albedo feedback mechanism. This mechanism is generally believed to be a key factor in amplifying natural variations within the earth s climate system. To achieve this understanding, we need to learn how shortwave radiation is absorbed and distributed in the ice pack and upper ocean, then assess the effects of this distribution on the regional heat and mass balance of the ice cover. Complicating the problem are a variety of issues related to the extreme sub-grid scale variability of the Arctic ice cover and to how such variability can be accounted for in large-scale models. Our long-term goal is to develop accurate formulations of the major ice-albedo feedback processes which are suitable for inclusion in climate and general circulation models. The original document contains color images. Text albedo Arctic Basin Arctic Arctic Ocean Ice permafrost 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 Atmospheric Physics
Physical and Dynamic Oceanography
Snow
Ice and Permafrost
Optics
*ALBEDO
*OCEAN BASINS
*PACK ICE
ARCTIC OCEAN
CLIMATE
DISTRIBUTION
FEEDBACK
HEAT BALANCE
PHYSICAL PROPERTIES
RADIATION
SHORT WAVELENGTHS
*ICE-ALBEDO FEEDBACK
SHORTWAVE RADIATION
spellingShingle Atmospheric Physics
Physical and Dynamic Oceanography
Snow
Ice and Permafrost
Optics
*ALBEDO
*OCEAN BASINS
*PACK ICE
ARCTIC OCEAN
CLIMATE
DISTRIBUTION
FEEDBACK
HEAT BALANCE
PHYSICAL PROPERTIES
RADIATION
SHORT WAVELENGTHS
*ICE-ALBEDO FEEDBACK
SHORTWAVE RADIATION
Maykut, Gary A
Grenfell, Thomas C
Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin
topic_facet Atmospheric Physics
Physical and Dynamic Oceanography
Snow
Ice and Permafrost
Optics
*ALBEDO
*OCEAN BASINS
*PACK ICE
ARCTIC OCEAN
CLIMATE
DISTRIBUTION
FEEDBACK
HEAT BALANCE
PHYSICAL PROPERTIES
RADIATION
SHORT WAVELENGTHS
*ICE-ALBEDO FEEDBACK
SHORTWAVE RADIATION
description Our overall goal is to develop a quantitative understanding of processes that collectively make up the ice-albedo feedback mechanism. This mechanism is generally believed to be a key factor in amplifying natural variations within the earth s climate system. To achieve this understanding, we need to learn how shortwave radiation is absorbed and distributed in the ice pack and upper ocean, then assess the effects of this distribution on the regional heat and mass balance of the ice cover. Complicating the problem are a variety of issues related to the extreme sub-grid scale variability of the Arctic ice cover and to how such variability can be accounted for in large-scale models. Our long-term goal is to develop accurate formulations of the major ice-albedo feedback processes which are suitable for inclusion in climate and general circulation models. The original document contains color images.
author2 WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES
format Text
author Maykut, Gary A
Grenfell, Thomas C
author_facet Maykut, Gary A
Grenfell, Thomas C
author_sort Maykut, Gary A
title Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin
title_short Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin
title_full Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin
title_fullStr Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin
title_full_unstemmed Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin
title_sort experimental and theoretical studies of ice-albedo feedback processes in the arctic basin
publishDate 2001
url http://www.dtic.mil/docs/citations/ADA625918
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA625918
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre albedo
Arctic Basin
Arctic
Arctic Ocean
Ice
permafrost
genre_facet albedo
Arctic Basin
Arctic
Arctic Ocean
Ice
permafrost
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA625918
op_rights Approved for public release; distribution is unlimited.
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