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中国沙漠  2019, Vol. 39 Issue (3): 163-171    DOI: 10.7522/j.issn.1000-694X.2018.00084
    
中国季风边缘区全新世沙地演化及其驱动机制研究进展
薛文萍1,2, 靳鹤龄1, 刘冰1, 孙良英1, 刘振宇1,2
1. 中国科学院西北生态环境资源研究院 沙漠与沙漠化重点实验室, 甘肃 兰州 730000;
2. 中国科学院大学, 北京 100049
Advances in the Study of Sandy Land Evolution and Driving Mechanism in the Monsoonal Marg in Area in China during the Holocene Epoch
Xue Wenping1,2, Jin Heling1, Liu Bing1, Sun Liangying1, Liu Zhenyu1,2
1. Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China
 全文: PDF(4415 KB)  
摘要: 中国季风边缘区全新世沙地演化和气候变化自东向西具有明显差异性。东部科尔沁沙地、中部毛乌素沙地呈现典型三段式沙地演化过程,西部共和盆地呈现多阶段多反复的沙地演化特征。东部科尔沁沙地、中部毛乌素沙地气候变化也呈现三段式,西部共和盆地由于地域特征气候变化相对复杂。全新世气候突变事件对各区产生差异影响。太阳辐射强度控制的亚洲季风环流和有效湿度变化影响沙地演化过程。
关键词: 全新世沙地演化气候变化突变事件驱动机制    
Abstract: Study of the evolution and climatic variation in the monsoonal margin area in China during the Holocene epoch shows there are obviously differences from the east to the west. Firstly, a typical three-stage evolution process is presented in the eastern Horqin Sandy Land and central Mu Us Sandy Land, while the western Gonghe Basin is characterized by multi-stage evolution. Secondly, in the eastern Horqin Sandy Land and central Mu Us Sandy Land the climate change is also presented in three phases, while the change of the western Gonghe Basin is relatively complicated due to the regional features. Thirdly, the Holocene abrupt climate events have different effects on different regions. The Asian monsoon circulation controlled by the solar isolation and the change of the effective humidity has great influence on the sandy evolution.
Key words: Holocene Epoch    sandy land evolution    climatic change    abrupt events    driving mechanism
收稿日期: 2018-04-11 出版日期: 2019-06-10
ZTFLH:  P531  
基金资助: 国家自然科学基金项目(41671204,41501220,41271215)
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引用本文:

薛文萍, 靳鹤龄, 刘冰, 孙良英, 刘振宇. 中国季风边缘区全新世沙地演化及其驱动机制研究进展[J]. 中国沙漠, 2019, 39(3): 163-171.

Xue Wenping, Jin Heling, Liu Bing, Sun Liangying, Liu Zhenyu. Advances in the Study of Sandy Land Evolution and Driving Mechanism in the Monsoonal Marg in Area in China during the Holocene Epoch. Journal of Desert Research, 2019, 39(3): 163-171.

链接本文:

http://www.desert.ac.cn/CN/10.7522/j.issn.1000-694X.2018.00084        http://www.desert.ac.cn/CN/Y2019/V39/I3/163

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