| SIMULATION OF REGIONAL CLIMATE OVER CHINA WITH CHINESE REGIONAL CLIMATE MODEL |
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| 作者姓名： | Li Weiliang Gong Wei Chen Longxun Song Yukuan |
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| 作者单位： | Chinese Academy of Meteorological Sciences Beijing 100081，Chinese Academy of Meteorological Sciences，Beijing 100081，Chinese Academy of Meteorological Scierices，Beijing 100081，Chinese Academy of Meteorological Scierices，Beijing 100081 |
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| 摘 要： | In this paper,we present the results simulated with the Chinese regional climate model nestedin NCAR CCM1 GCM through one-way nesting approach.The model has been run for 14 months.The NCAR CCM1(1992)is at rhomboidal truncation(R15),while the horizontal resolution ofthe Chinese regional climate model is 100 km.It is found that the Chinese regional climate modelhas some advantages in simulating the surface air temperature and precipitation over the generalclimate model,because of the improved land surface parameterization.
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| 收稿时间： | 1996/4/25 0:00:00 |
| 修稿时间： | 1996/10/27 0:00:00 |
SIMULATION OF REGIONAL CLIMATE OVER CHINA WITH CHINESE REGIONAL CLIMATE MODEL |
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| Li Weiliang,Gong Wei,Chen Longxun,Song Yukuan.SIMULATION OF REGIONAL CLIMATE OVER CHINA WITH CHINESE REGIONAL CLIMATE MODEL[J].Acta Meteorologica Sinica,1997,11(3):307-319. |
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| Authors: | Li Weiliang Gong Wei Chen Longxun and Song Yukuan |
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| Institution: | Li Weiliang Gong Wei Chen Longxun Song Yukuan Chinese Academy of Meteorological Sciences,Beijing 100081 |
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| Abstract: | In this paper,we present the results simulated with the Chinese regional climate model nested in NCAR CCM1 GCM through one-way nesting approach.The model has been run for 14 months. The NCAR CCM1(1992)is at rhomboidal truncation(R15),while the horizontal resolution of the Chinese regional climate model is 100 km.It is found that the Chinese regional climate model has some advantages in simulating the surface air temperature and precipitation over the general climate model,because of the improved land surface parameterization. |
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| Keywords: | regional climate one way nesting simulation seasonal change |
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