2006
DOI: 10.1002/ldr.744
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Hydrological changes and land degradation in the southern and eastern Tarim basin, Xinjiang, China

Abstract: Using the combined methods of digital image processing of remote sensing data, a Geographical Information System (GIS) and analysis of historical books and maps, this paper aims to contribute to a better understanding of the processes and mechanisms of land-use and land-cover changes and hydrological variations during the last 2000 years in a hyper-arid environment. The southern and eastern Taklamakan Desert, one of the driest and ecologically most sensitive regions in China and characterized by a long history… Show more

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Cited by 57 publications
(49 citation statements)
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“…One can note that this timeline is coincident with the cooldry tendency of climate shown in Fig. 5 (Wang, 1998;Yang et al, 2006).…”
Section: Human History and The Abandonment Of Settlementssupporting
confidence: 61%
“…One can note that this timeline is coincident with the cooldry tendency of climate shown in Fig. 5 (Wang, 1998;Yang et al, 2006).…”
Section: Human History and The Abandonment Of Settlementssupporting
confidence: 61%
“…The human impact on the landscape of the desert margins of northwest China during the last 2000 yr is clearly visible in the remains of ruined cities and abandoned settlements (e.g., Huang, 1958;Huang, 2003;Yang et al, 2006a). Nomadic activity, i.e., Qijia Culture (ca.…”
Section: Discussionmentioning
confidence: 99%
“…Formation of river terraces and change in the length of the Keriya River, coupled with historical records detailing the distribution of the water bodies (Yang et al, 2006a), suggest that wetlands (rivers and lakes) were much more extensive at ca. 2 ka and during the Little Ice Age in the Taklamakan Desert.…”
Section: The Holocene Periodmentioning
confidence: 99%
“…The Taklimakan Desert is the world's second largest active sand desert. It covers an area of 338,000 km 2 , and as much as 85 percent of it consists of active sand dunes [6,7] . Many researchers believe that the Taklamakan Desert was originally formed in the centre of the Tarim Basin as early as the Tertiary Period and then the desert expanded outwards [8] .…”
Section: Study Areamentioning
confidence: 99%