Detection and Attribution of Regional Climate Change

We developed a high resolution global coupled modeling capability to perform breakthrough studies of the regional climate change. The atmospheric component in our simulation uses a 1{sup o} latitude x 1.25{sup o} longitude grid which is the finest resolution ever used for the NCAR coupled climate mo...

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Main Authors: Bala, G., Mirin, A.
Other Authors: United States. Department of Energy.
Format: Report
Language:English
Published: Lawrence Livermore National Laboratory 2007
Subjects:
Online Access:https://doi.org/10.2172/1036845
https://digital.library.unt.edu/ark:/67531/metadc834490/
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spelling ftunivnotexas:info:ark/67531/metadc834490 2023-05-15T13:45:29+02:00 Detection and Attribution of Regional Climate Change Bala, G. Mirin, A. United States. Department of Energy. 2007-01-19 PDF-file: 19 pages; size: 0.6 Mbytes Text https://doi.org/10.2172/1036845 https://digital.library.unt.edu/ark:/67531/metadc834490/ English eng Lawrence Livermore National Laboratory rep-no: UCRL-TR-227391 grantno: W-7405-ENG-48 doi:10.2172/1036845 osti: 1036845 https://digital.library.unt.edu/ark:/67531/metadc834490/ ark: ark:/67531/metadc834490 Lawrence Livermore National Laboratory Testing Oceanography Validation Seas Thickness 58 Geosciences Detection 54 Environmental Sciences Configuration Simulation Distribution Resolution Climate Models Climates Report 2007 ftunivnotexas https://doi.org/10.2172/1036845 2021-03-20T23:08:01Z We developed a high resolution global coupled modeling capability to perform breakthrough studies of the regional climate change. The atmospheric component in our simulation uses a 1{sup o} latitude x 1.25{sup o} longitude grid which is the finest resolution ever used for the NCAR coupled climate model CCSM3. Substantial testing and slight retuning was required to get an acceptable control simulation. The major accomplishment is the validation of this new high resolution configuration of CCSM3. There are major improvements in our simulation of the surface wind stress and sea ice thickness distribution in the Arctic. Surface wind stress and ocean circulation in the Antarctic Circumpolar Current are also improved. Our results demonstrate that the FV version of the CCSM coupled model is a state of the art climate model whose simulation capabilities are in the class of those used for IPCC assessments. We have also provided 1000 years of model data to Scripps Institution of Oceanography to estimate the natural variability of stream flow in California. In the future, our global model simulations will provide boundary data to high-resolution mesoscale model that will be used at LLNL. The mesoscale model would dynamically downscale the GCM climate to regional scale on climate time scales. Report Antarc* Antarctic Arctic Climate change Sea ice University of North Texas: UNT Digital Library Antarctic Arctic Scripps ENVELOPE(-63.783,-63.783,-69.150,-69.150) The Antarctic
institution Open Polar
collection University of North Texas: UNT Digital Library
op_collection_id ftunivnotexas
language English
topic Lawrence Livermore National Laboratory
Testing
Oceanography
Validation
Seas
Thickness
58 Geosciences
Detection
54 Environmental Sciences
Configuration
Simulation
Distribution
Resolution
Climate Models
Climates
spellingShingle Lawrence Livermore National Laboratory
Testing
Oceanography
Validation
Seas
Thickness
58 Geosciences
Detection
54 Environmental Sciences
Configuration
Simulation
Distribution
Resolution
Climate Models
Climates
Bala, G.
Mirin, A.
Detection and Attribution of Regional Climate Change
topic_facet Lawrence Livermore National Laboratory
Testing
Oceanography
Validation
Seas
Thickness
58 Geosciences
Detection
54 Environmental Sciences
Configuration
Simulation
Distribution
Resolution
Climate Models
Climates
description We developed a high resolution global coupled modeling capability to perform breakthrough studies of the regional climate change. The atmospheric component in our simulation uses a 1{sup o} latitude x 1.25{sup o} longitude grid which is the finest resolution ever used for the NCAR coupled climate model CCSM3. Substantial testing and slight retuning was required to get an acceptable control simulation. The major accomplishment is the validation of this new high resolution configuration of CCSM3. There are major improvements in our simulation of the surface wind stress and sea ice thickness distribution in the Arctic. Surface wind stress and ocean circulation in the Antarctic Circumpolar Current are also improved. Our results demonstrate that the FV version of the CCSM coupled model is a state of the art climate model whose simulation capabilities are in the class of those used for IPCC assessments. We have also provided 1000 years of model data to Scripps Institution of Oceanography to estimate the natural variability of stream flow in California. In the future, our global model simulations will provide boundary data to high-resolution mesoscale model that will be used at LLNL. The mesoscale model would dynamically downscale the GCM climate to regional scale on climate time scales.
author2 United States. Department of Energy.
format Report
author Bala, G.
Mirin, A.
author_facet Bala, G.
Mirin, A.
author_sort Bala, G.
title Detection and Attribution of Regional Climate Change
title_short Detection and Attribution of Regional Climate Change
title_full Detection and Attribution of Regional Climate Change
title_fullStr Detection and Attribution of Regional Climate Change
title_full_unstemmed Detection and Attribution of Regional Climate Change
title_sort detection and attribution of regional climate change
publisher Lawrence Livermore National Laboratory
publishDate 2007
url https://doi.org/10.2172/1036845
https://digital.library.unt.edu/ark:/67531/metadc834490/
long_lat ENVELOPE(-63.783,-63.783,-69.150,-69.150)
geographic Antarctic
Arctic
Scripps
The Antarctic
geographic_facet Antarctic
Arctic
Scripps
The Antarctic
genre Antarc*
Antarctic
Arctic
Climate change
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Climate change
Sea ice
op_relation rep-no: UCRL-TR-227391
grantno: W-7405-ENG-48
doi:10.2172/1036845
osti: 1036845
https://digital.library.unt.edu/ark:/67531/metadc834490/
ark: ark:/67531/metadc834490
op_doi https://doi.org/10.2172/1036845
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