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Application of Supercomputer in Simulating the Asian Climate Using High-resolution Numerical Model

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dc.contributor.authorKim, Seong-Joong-
dc.date.issued2007-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/7721-
dc.description.abstractUnder the framework of an IBM power-4 supercomputer, the Asian climate was simulated using a high-resolution atmospheric general circulation model, the NCAR CCM3 at spectral truncation of T170 corresponding to a grid cell size of roughly 75 km. To assess whether there are significant benefits from the high-resolution model compared to a lower-resolution model result, a T42 model was applied for the climate simulation with identical boundary conditions. Both model versions capture the modern climate features found in the observation reasonably well, but the high-resolution model results appear to be more realistic. The high-resolution model is especially useful in reproducing regional-scale climate features such as Asian Monsoon, which has a huge socio-economic impact. In predicting future climate change, thus, an applicaion of a high-resolution numerical model is desirable.-
dc.languageEnglish-
dc.titleApplication of Supercomputer in Simulating the Asian Climate Using High-resolution Numerical Model-
dc.title.alternative고해상도 수치 모델을 이용하여 아시아 기후 시뮬레이션시 슈퍼컴퓨터의 적용-
dc.typeProceeding-
dc.identifier.bibliographicCitationKim, Seong-Joong. 2007. Application of Supercomputer in Simulating the Asian Climate Using High-resolution Numerical Model. 한국과학기술정보연구원. 한국과학기술정보연구원. 2007.09.11~.-
dc.citation.volume1-
dc.citation.number1-
dc.citation.conferenceDate2007.09.11~-
dc.citation.conferenceName한국과학기술정보연구원-
dc.citation.conferencePlace한국과학기술정보연구원-
dc.description.articleClassificationPro(FULL)국제-
dc.subject.keywordAsian Climate-
dc.subject.keywordHigh-resolution Numerical Mode-
dc.subject.keywordsupercomputer-
dc.identifier.localId2007-0094-
Appears in Collections  
2007-2010, Integrated research on the COMposition of Polar Atmosphere and Climate Change(COMPAC) (07-10) / Lee, Bang Yong
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