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《ACTA MICROPALAEONTOLOGICA SINICA》 2000-02
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STUDIES OF THE CLIMATIC DYNAMICS FOR THE MID- HOLOCENE VEGETATIONAL CHANGES IN CHINA

Yu Ge and Wang Su min (Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008)  
The orbit forcing theory suggests that the insolation at 6ka was lower than at the present in winter season in low and middle latitudes. This driving climate has been simulated by palaeo GCMs showing a lower than present winter temperature in East Asian. The palaeoclimate driven vegetation has been simulated by biome models showing the mid Holocene forest vegetation was shifted southwards in China. However, the palaeovegetation reconstructed by a great of pollen records displays the forest zones migration systematically northwards when compared with the present. These vegetation patterns are used to furthermore reconstructed the climate which reflect a warmer than present winter in China. As there existed huge different or contrasting results between geological observations and model simulations, we recognized that dynamic mechanisms can not be only limited in the orbit forcing. The land surface feedback in Asian monsoon regions could play a greater important role than direct insolation anomaly.
【CateGory Index】: Q911.59
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