| Desert and Desertification |
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| Responses of Desertification to Climate Change in Arid and Semiarid Regions of China Over the Past Millennium |
| HUA Ting1, WANG Xun-ming1, Cizhen2, ZHANG Cai-xia1, LANG Li-li1 |
| 1.Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China; 2.Lhasa Meteorological Bureau, Lhasa 850000, China |
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Abstract Most of the arid and semiarid regions in China have experienced multiple arid phases throughout the Quaternary, and they are highly sensitive to climate change. However, the response of desertification to climate change is poorly understood. In the present study, we selected multiple climatic proxies and desertification evidences to estimate the responses of desertification to climate changes in arid and semiarid regions of China over the past millennium. Desertification generally decreased in western China during the Little Ice Age (LIA), but increased during the Medieval Warm Period (MWP) and the Current Warm Period (CWP), which suggested the environment in western China was inclined to meliorate in cold period and deteriorate in warm period. The central and eastern regions of China tended to experience desertification in LIA, but desertification reversed in MWP and CWP, which indicated the central and eastern regions of China were prone to undergo desertification in cold period but desertification reversed in warm period. However, the desertification cycles in the Qinghai-Tibetan Plateau region showed fluctuation responding to climate change.
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Received: 10 August 2011
Published: 20 May 2012
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2012, Vol. 32 
