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 major factor in amplifying variations that occur within the earth's climate system. To achieve this understanding, w...

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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: 1998
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA541968
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA541968
id ftdtic:ADA541968
record_format openpolar
spelling ftdtic:ADA541968 2023-05-15T13:10:29+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 1998-09-30 text/html http://www.dtic.mil/docs/citations/ADA541968 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA541968 en eng http://www.dtic.mil/docs/citations/ADA541968 Approved for public release; distribution is unlimited. DTIC Astrophysics Physical and Dynamic Oceanography Snow Ice and Permafrost *ARCTIC OCEAN *PACK ICE *OCEAN BASINS *SOLAR RADIATION CLIMATE HEAT EARTH(PLANET) CIRCULATION SHORT WAVELENGTHS ARCTIC REGIONS BALANCE ICE FORMATION THEORY EXPERIMENTAL DATA MODELS Text 1998 ftdtic 2016-02-23T07:27:31Z 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 major factor in amplifying variations that occur 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 Arctic 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. Ultimately, we plan to develop and test appropriate techniques for accurately incorporating ice-albedo feedback into climate and general circulation models. See also ADM002252. 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 Astrophysics
Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ARCTIC OCEAN
*PACK ICE
*OCEAN BASINS
*SOLAR RADIATION
CLIMATE
HEAT
EARTH(PLANET)
CIRCULATION
SHORT WAVELENGTHS
ARCTIC REGIONS
BALANCE
ICE FORMATION
THEORY
EXPERIMENTAL DATA
MODELS
spellingShingle Astrophysics
Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ARCTIC OCEAN
*PACK ICE
*OCEAN BASINS
*SOLAR RADIATION
CLIMATE
HEAT
EARTH(PLANET)
CIRCULATION
SHORT WAVELENGTHS
ARCTIC REGIONS
BALANCE
ICE FORMATION
THEORY
EXPERIMENTAL DATA
MODELS
Maykut, Gary A.
Grenfell, Thomas C.
Experimental and Theoretical Studies of Ice-Albedo Feedback Processes in the Arctic Basin
topic_facet Astrophysics
Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*ARCTIC OCEAN
*PACK ICE
*OCEAN BASINS
*SOLAR RADIATION
CLIMATE
HEAT
EARTH(PLANET)
CIRCULATION
SHORT WAVELENGTHS
ARCTIC REGIONS
BALANCE
ICE FORMATION
THEORY
EXPERIMENTAL DATA
MODELS
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 major factor in amplifying variations that occur 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 Arctic 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. Ultimately, we plan to develop and test appropriate techniques for accurately incorporating ice-albedo feedback into climate and general circulation models. See also ADM002252.
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 1998
url http://www.dtic.mil/docs/citations/ADA541968
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA541968
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/ADA541968
op_rights Approved for public release; distribution is unlimited.
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