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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| Veröffentlicht in: | Atmospheric science letters 2011-04, Vol.12 (2), p.213-219 |
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| container_end_page | 219 |
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| container_title | Atmospheric science letters |
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| creator | Chotamonsak, Chakrit Salathé, Eric P. Kreasuwan, Jiemjai Chantara, Somporn Siriwitayakorn, Kingkeo |
| description | 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. Copyright © 2011 Royal Meteorological Society |
| doi_str_mv | 10.1002/asl.313 |
| format | Article |
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| source | Wiley Online Library (Open Access Collection) |
| subjects | Bias Climate change Climate models Climate science Dry season dynamical downscaling General circulation models Global climate Global climate models Maximum temperatures Minimum temperatures Ocean circulation Precipitation regional climate model Regional climate models Regional climates Seasons Simulation Southeast Asia Spatial distribution Temperature distribution Wind |
| title | Projected climate change over Southeast Asia simulated using a WRF regional climate model |
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