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试论全球气候变化与沙漠化的关系
引用本文:董光荣,申建友,金炯.试论全球气候变化与沙漠化的关系[J].第四纪研究,1990,10(1):91-98.
作者姓名:董光荣  申建友  金炯
作者单位:中国科学院兰州沙漠研究所(董光荣),中国科学院西安黄土与第四纪地质开放研究实验室(申建友)
摘    要:本文通过全球气候变化对沙漠化的影响和沙漠化对沙区气候的反馈作用两方面,论述在气候变暖条件下,全球气候变化与沙漠化的关系,例如我国东部沙区降水增多,沙漠化逆转,西部沙区降水减少,沙漠化发展等原因。

关 键 词:全球气候变化  沙漠化  反馈作用

ON THE RELATIONSHIP BETWEEN THE GLOBAL CLIMATE CHANGE AND DESERTIFICATION
Institution:1. Lanzhon Institute of Desert Research, Chinese Academy of Sciences;
2. Xian Laboratory of Loess and Quaternary Geology,Chinese Academy of Sciences
Abstract:Synthesizing the available data at home and abroad, the authors concluded that the global climate change controlls the desertification and de-desertification by its effect on the variation in dry-wet climate over sand area; on the other hand, the desertification and de-desertification have a feedback effect on global climate change in the way of its impact on the radiation equilibrium, condensation nucleus, moisture and convection. If the global climate became warming due to the man-made CO2 and other greenhouse effect gases, the developing tendencies of desertification in northern China sand area would be that when the precipitation in the eastern China sand area increased, the desertification process would be retarded, even reversed; and the precipitation in western China decreased, the desertification would be accelerated.Today's climate is substantially a result of coupling anthropogenic and natural climate. In the geological time, the recent stage and the future, natural climate must be a dominant part of the climatic factors and less of anthropogenic factors. The natural climate always fluctuates in diffierent periods and amplitudes, while the anthropogenic climate characterized by greenhouse effect of man-made CO2 and other trace gases would be linearly or exponentially varied. So the coupling of two parts——climate regime (such as temperature) occurred in a given time will have three potential situations rather than one: when natural change corresponds to the anthropogenic, the temperature will rise greatly; if the natural change is contrary to the anthropogenic and the former amplitude is greater than the latter, the temperature will drop, but slightly; if the natural change opposes the anthropogenic and the former amplitude is equal to the latter, the temperature will remain the same. Since the tendencies of natural change are uncertain so far, it is impossible to determine the trends of global climate change due to increasing anthropogenic greenhouse effect. The authors proposed that we must strengthen the study of natural climate change in the research of CO2 greenhouse effect.
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