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이용수
1. Introduction
2. Model
3. Results
Acknowledgement
Reference
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The Effects of Horizontal Resolution on East Asian Summer Monsoon Simulations by CMIP5 AGCMs
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FUTURE CHANGES OF ASIAN MONSOON SIMULATED BY HIGH-RESOLUTION MRI-AGCM
한국기상학회 학술대회 논문집
2011 .10
Simulation of the east Asian summer monsoon in a high-resolution regional climate model
한국기상학회 학술대회 논문집
2006 .10
A Study of the Asian Summer Monsoon and 1997/98 ENSO-Monsoon Interaction in AGCM Intercomparison
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2000 .10
Predictability of Interannual Variability of East Asian Summer Monsoon with the Use of Ensembles by AGCM
한국기상학회 학술대회 논문집
2005 .04
Studies on the Variability and Prediction of East Asian Summer Monsoon
Korean Journal of the Atmospheric Sciences
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Characterizing the multi-stage evolution of interannual East Asian summer monsoon variability
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Responses of Asian summer monsoon duration to different global temperature targets
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The Aerosol Effect on Radiation and Monsoon Circulation : AGCM Study
대기
2003 .10
VERIFICATION OF ASIAN-AUSTRALIAN MONSOON SIMULATED BY AGCMS AND APPLICATION OF STATISTICAL DOWNSCALING TO PRODUCE REGIONAL MONSOON VARIABILITY
대기
2002 .04
A numerical study on the East Asian summer monsoon and precipitation over China
한국기상학회 학술대회 논문집
2006 .10
High-resolution Simulation of the Asian Monsoon at 6000 Years BP
제4기학회지
2005 .01
RECENT WEAKENING OF EAST ASIAN SUMMER MONSOON : A POSSIBLE RESPONSE TO GLOBAL WARMING
한국기상학회 학술대회 논문집
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Evaluation of the East Asian Monsoon Simulation in Climate Models
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Numerical Simulation of the Asian Monsoon and the Global Water Cycle
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1996 .04
Linkages between the South and East Asian summer monsoons : A review and revisit
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East Asian precipitation change in the future climate simulated by a 20㎞-AGCM
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2007 .04
An assessment of future climatic changes of the East Asian summer monsoon using AR4 coupled climate models
한국기상학회 학술대회 논문집
2011 .10
Atmospheric rivers in East Asian summer monsoon: Subseasonal variability and their hydrological impacts
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2019 .10
AGCM의 수평세밀격자화에 따른 반응 연구
Asia-Pacific Journal of Atmospheric Sciences
1996 .08
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