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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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 |
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Open Polar |
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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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1766230642102632448 |