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. Central to achieving this understandi...

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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: 2003
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA615526
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA615526
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spelling ftdtic:ADA615526 2023-05-15T13:10:31+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 2003-09-30 text/html http://www.dtic.mil/docs/citations/ADA615526 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA615526 en eng http://www.dtic.mil/docs/citations/ADA615526 Approved for public release; distribution is unlimited. DTIC Meteorology Snow Ice and Permafrost *ALBEDO *FEEDBACK *SEA ICE ARCTIC OCEAN CLIMATE CLIMATE CHANGE HEAT FLUX ICE FORMATION MASS MELTING PACK ICE SEASONAL VARIATIONS SUMMER THICKNESS ICE COVER ICE MASS BALANCE ICE PACK MASS FLUX MELT PONDS SHORTWAVE RADIATION SURFACE MELT WATER UPPER OCEAN Text 2003 ftdtic 2016-02-24T17:35:13Z 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. Central to achieving this understanding is learning more about how shortwave radiation is absorbed and distributed in the ice pack and upper ocean, and how this distribution affects 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 major ice-albedo feedback processes in a form suitable for inclusion in climate and general circulation models. Text albedo Arctic Basin Arctic Arctic Ocean Climate change Ice ice pack permafrost Sea ice 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 Meteorology
Snow
Ice and Permafrost
*ALBEDO
*FEEDBACK
*SEA ICE
ARCTIC OCEAN
CLIMATE
CLIMATE CHANGE
HEAT FLUX
ICE FORMATION
MASS
MELTING
PACK ICE
SEASONAL VARIATIONS
SUMMER
THICKNESS
ICE COVER
ICE MASS BALANCE
ICE PACK
MASS FLUX
MELT PONDS
SHORTWAVE RADIATION
SURFACE MELT WATER
UPPER OCEAN
spellingShingle Meteorology
Snow
Ice and Permafrost
*ALBEDO
*FEEDBACK
*SEA ICE
ARCTIC OCEAN
CLIMATE
CLIMATE CHANGE
HEAT FLUX
ICE FORMATION
MASS
MELTING
PACK ICE
SEASONAL VARIATIONS
SUMMER
THICKNESS
ICE COVER
ICE MASS BALANCE
ICE PACK
MASS FLUX
MELT PONDS
SHORTWAVE RADIATION
SURFACE MELT WATER
UPPER OCEAN
Maykut, Gary A
Grenfell, Thomas C
Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin
topic_facet Meteorology
Snow
Ice and Permafrost
*ALBEDO
*FEEDBACK
*SEA ICE
ARCTIC OCEAN
CLIMATE
CLIMATE CHANGE
HEAT FLUX
ICE FORMATION
MASS
MELTING
PACK ICE
SEASONAL VARIATIONS
SUMMER
THICKNESS
ICE COVER
ICE MASS BALANCE
ICE PACK
MASS FLUX
MELT PONDS
SHORTWAVE RADIATION
SURFACE MELT WATER
UPPER OCEAN
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. Central to achieving this understanding is learning more about how shortwave radiation is absorbed and distributed in the ice pack and upper ocean, and how this distribution affects 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 major ice-albedo feedback processes in a form suitable for inclusion in climate and general circulation models.
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 2003
url http://www.dtic.mil/docs/citations/ADA615526
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA615526
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre albedo
Arctic Basin
Arctic
Arctic Ocean
Climate change
Ice
ice pack
permafrost
Sea ice
genre_facet albedo
Arctic Basin
Arctic
Arctic Ocean
Climate change
Ice
ice pack
permafrost
Sea ice
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA615526
op_rights Approved for public release; distribution is unlimited.
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