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High-resolution simulation of the global climate and Asian monsoon at 6000 years BP

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Title
High-resolution simulation of the global climate and Asian monsoon at 6000 years BP
Other Titles
고해상도 기후모델을 이용한 6000년전의 아시아 몬순재현 시뮬레이션
Authors
Kim, Seong-Joong
David Erickson
Phil Duffy
Balla Govindasamy
Tom Crowley
Keywords
ccm3climatehigh-resolutionmonsoonsimulation
Issue Date
2005
Citation
Kim, Seong-Joong, et al. 2005. High-resolution simulation of the global climate and Asian monsoon at 6000 years BP. American Geophysical Union. American Geophysical Union. 2005.12.05~.
Abstract
The change in the global climate and the Asian monsoon during the mid-Holocene, 6000 years before present (6ka), is simulated by a high-resolution climate model at spectral truncations of T170, corresponding to grid cell sizes of roughly 75 km. The present simulation was forced with observed monthly sea surface temperatures, and specified atmospheric carbon dioxide concentration, while in the mid-Holocene experiment, orbital parameters (obliquity, precession, and eccentricity) were changed to 6ka. With the 6ka conditions, the precipitation associated with the summer monsoon is enhanced over wider zonal band from the middle-east to Southeast Asia, while in winter precipitation wasn't much altered. The monsoonal wind also increases over the Arabian Sea showing the enhanced southwest wind during the summer and the north east wind during the winter. Overall, the high-resolution simulation captures detailed features of the Asian monsoon and its strength is enhanced during the mid-Holocene, especially in summer, consistent with other previous model simulations.
URI
https://repository.kopri.re.kr/handle/201206/7601
Conference Name
American Geophysical Union
Conference Place
American Geophysical Union
Conference Date
2005.12.05~
Type
Proceeding
Indexed
Pro(초록)국외
Appears in Collections  
2004-2005, A Study on the Arctic Environmental Characteristics (04-05) / Lee, Bang Yong (PP04108, PE05007)
2004-2006, 아시아 몬순순화 재현 수치실험 (04-06) / Kim, Seong-Joong (PG05020, PG04001)
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