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《大气科学进展(英文版)》 2000-03
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The Seasonal Climate and Low Frequency Oscillation in the Simulated Mid-Holocene Megathermal Climate

Wang Hujun (LASG, Institute of Atmopheric Physics, Chinese Academy of Sciences. Beijing 100029)  
The mid-Holocene climate about 6000 years ago was simulated by using the atmospheric general circulation model. The orbital parameters for 6 ka BP (before present) were prescribed and other forcing factorswere set in the modern conditions. Results show that the large-scale climate change in the Aflican-Asianmonsoon areas during the summer-time is strongly compared to the present climate. while the changes inother seasons and regions are generally weak. The results also revealed the change of the low frequencyoscillation in the atmosphere.
【CateGory Index】: P46
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