Towards Prediction of Environmental Arctic Change

Our main objective is to use models of the coupled ice-ocean Arctic environment to understand the past and present sea ice and ocean states and to predict future scenarios of environmental change in the Arctic Ocean. To meet this objective we have developed a coupled ice-ocean model of the sea ice c...

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Main Author: Maslowski, Wieslaw
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA
Format: Text
Language:English
Published: 2004
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADP023853
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADP023853
id ftdtic:ADP023853
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spelling ftdtic:ADP023853 2023-05-15T14:36:26+02:00 Towards Prediction of Environmental Arctic Change Maslowski, Wieslaw NAVAL POSTGRADUATE SCHOOL MONTEREY CA 2004-06 text/html http://www.dtic.mil/docs/citations/ADP023853 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADP023853 en eng http://www.dtic.mil/docs/citations/ADP023853 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography Numerical Mathematics *ARCTIC REGIONS *ARCTIC OCEAN *MATHEMATICAL PREDICTION *MATHEMATICAL MODELS SEA ICE GREENHOUSE EFFECT SALINITY OCEANOGRAPHIC DATA ENVIRONMENTS SYMPOSIA HEATING *WARMING COMPONENT REPORTS Text 2004 ftdtic 2016-02-22T17:59:32Z Our main objective is to use models of the coupled ice-ocean Arctic environment to understand the past and present sea ice and ocean states and to predict future scenarios of environmental change in the Arctic Ocean. To meet this objective we have developed a coupled ice-ocean model of the sea ice covered northern hemisphere at 9-km and 45-level grid. The model has been spun up for 48 years. Three 24-year experiments have been completed following the spin up, all forced with realistic 1979-2002 ECMWF data but with a different surface temperature and salinity restoring times. Results from these integrations are compared to each other and to sea ice data available over this period to address the growing need for understanding the recent warming and the subsequent decrease of the Arctic Ice Pack during the late 1990s and 2000s. Presented at the DoD High Performance Computing Modernization Program (HPCMP) Users Group Conference (UGC), held in Williamsburg, Virginia on 7-11 June 2004. The original document contains color images. All DTIC reproductions will be in black and white. This article is from ADA492363 Proceedings of the HPCMP Users Group Conference 2004. Text Arctic Arctic Ocean ice pack 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 Physical and Dynamic Oceanography
Numerical Mathematics
*ARCTIC REGIONS
*ARCTIC OCEAN
*MATHEMATICAL PREDICTION
*MATHEMATICAL MODELS
SEA ICE
GREENHOUSE EFFECT
SALINITY
OCEANOGRAPHIC DATA
ENVIRONMENTS
SYMPOSIA
HEATING
*WARMING
COMPONENT REPORTS
spellingShingle Physical and Dynamic Oceanography
Numerical Mathematics
*ARCTIC REGIONS
*ARCTIC OCEAN
*MATHEMATICAL PREDICTION
*MATHEMATICAL MODELS
SEA ICE
GREENHOUSE EFFECT
SALINITY
OCEANOGRAPHIC DATA
ENVIRONMENTS
SYMPOSIA
HEATING
*WARMING
COMPONENT REPORTS
Maslowski, Wieslaw
Towards Prediction of Environmental Arctic Change
topic_facet Physical and Dynamic Oceanography
Numerical Mathematics
*ARCTIC REGIONS
*ARCTIC OCEAN
*MATHEMATICAL PREDICTION
*MATHEMATICAL MODELS
SEA ICE
GREENHOUSE EFFECT
SALINITY
OCEANOGRAPHIC DATA
ENVIRONMENTS
SYMPOSIA
HEATING
*WARMING
COMPONENT REPORTS
description Our main objective is to use models of the coupled ice-ocean Arctic environment to understand the past and present sea ice and ocean states and to predict future scenarios of environmental change in the Arctic Ocean. To meet this objective we have developed a coupled ice-ocean model of the sea ice covered northern hemisphere at 9-km and 45-level grid. The model has been spun up for 48 years. Three 24-year experiments have been completed following the spin up, all forced with realistic 1979-2002 ECMWF data but with a different surface temperature and salinity restoring times. Results from these integrations are compared to each other and to sea ice data available over this period to address the growing need for understanding the recent warming and the subsequent decrease of the Arctic Ice Pack during the late 1990s and 2000s. Presented at the DoD High Performance Computing Modernization Program (HPCMP) Users Group Conference (UGC), held in Williamsburg, Virginia on 7-11 June 2004. The original document contains color images. All DTIC reproductions will be in black and white. This article is from ADA492363 Proceedings of the HPCMP Users Group Conference 2004.
author2 NAVAL POSTGRADUATE SCHOOL MONTEREY CA
format Text
author Maslowski, Wieslaw
author_facet Maslowski, Wieslaw
author_sort Maslowski, Wieslaw
title Towards Prediction of Environmental Arctic Change
title_short Towards Prediction of Environmental Arctic Change
title_full Towards Prediction of Environmental Arctic Change
title_fullStr Towards Prediction of Environmental Arctic Change
title_full_unstemmed Towards Prediction of Environmental Arctic Change
title_sort towards prediction of environmental arctic change
publishDate 2004
url http://www.dtic.mil/docs/citations/ADP023853
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADP023853
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
ice pack
Sea ice
genre_facet Arctic
Arctic Ocean
ice pack
Sea ice
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADP023853
op_rights Approved for public release; distribution is unlimited.
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