Projected climate change over Southeast Asia simulated using a WRF regional climate model
Dynamical downscaling of a global climate model is applied at 60-km horizontal resolution to project changes from 1990-1999 to 2045-2054 of temperature and precipitation over Southeast Asia. The regional climate model reproduces the observed spatial distribution of temperature well, with a cold bias...
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th-cmuir.6653943832-499052018-09-04T04:20:05Z Projected climate change over Southeast Asia simulated using a WRF regional climate model Chakrit Chotamonsak Eric P. Salathé Jiemjai Kreasuwan Somporn Chantara Kingkeo Siriwitayakorn Earth and Planetary Sciences Dynamical downscaling of a global climate model is applied at 60-km horizontal resolution to project changes from 1990-1999 to 2045-2054 of temperature and precipitation over Southeast Asia. The regional climate model reproduces the observed spatial distribution of temperature well, with a cold bias for maximum temperatures and a warm bias for minimum temperatures. Wet-season precipitation is simulated with less skill than dry-season precipitation. Projected warming varies from < 0.1 to 3 °C depending on the location and season, with greater warming at night than daytime for all seasons. Precipitation increases on average, with local decreases in the dry season. © 2011 Royal Meteorological Society. 2018-09-04T04:20:05Z 2018-09-04T04:20:05Z 2011-04-01 Journal 1530261X 2-s2.0-79954608654 10.1002/asl.313 https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=79954608654&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/49905 |
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Earth and Planetary Sciences Chakrit Chotamonsak Eric P. Salathé Jiemjai Kreasuwan Somporn Chantara Kingkeo Siriwitayakorn Projected climate change over Southeast Asia simulated using a WRF regional climate model |
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Dynamical downscaling of a global climate model is applied at 60-km horizontal resolution to project changes from 1990-1999 to 2045-2054 of temperature and precipitation over Southeast Asia. The regional climate model reproduces the observed spatial distribution of temperature well, with a cold bias for maximum temperatures and a warm bias for minimum temperatures. Wet-season precipitation is simulated with less skill than dry-season precipitation. Projected warming varies from < 0.1 to 3 °C depending on the location and season, with greater warming at night than daytime for all seasons. Precipitation increases on average, with local decreases in the dry season. © 2011 Royal Meteorological Society. |
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author |
Chakrit Chotamonsak Eric P. Salathé Jiemjai Kreasuwan Somporn Chantara Kingkeo Siriwitayakorn |
author_facet |
Chakrit Chotamonsak Eric P. Salathé Jiemjai Kreasuwan Somporn Chantara Kingkeo Siriwitayakorn |
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Chakrit Chotamonsak |
title |
Projected climate change over Southeast Asia simulated using a WRF regional climate model |
title_short |
Projected climate change over Southeast Asia simulated using a WRF regional climate model |
title_full |
Projected climate change over Southeast Asia simulated using a WRF regional climate model |
title_fullStr |
Projected climate change over Southeast Asia simulated using a WRF regional climate model |
title_full_unstemmed |
Projected climate change over Southeast Asia simulated using a WRF regional climate model |
title_sort |
projected climate change over southeast asia simulated using a wrf regional climate model |
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2018 |
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https://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=79954608654&origin=inward http://cmuir.cmu.ac.th/jspui/handle/6653943832/49905 |
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