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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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 |
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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. |
_version_ |
1766232368260055040 |