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车尔臣河下游自1989年改道以来,河道北边形成若干小湖,使台特玛湖-康拉克地区的水域格局发生了很大变化.干涸30多年的台特玛湖,随着自2000年起塔里木河下游应急生态输水工程的实施开始形成大片水域,且水域面积呈扩大趋势.2002年车尔臣河改道结束后康拉克地区的湖泊格局基本形成,而台特玛湖地区的水域则继续大幅变化.本文在1972-2012年102期遥感影像及其相关辅助数据基础上进行各项定量分析,详细描述台特玛湖-康拉克地区的水域变化过程,总结变化趋势,试图找出变化主导因素.笔者认为台特玛湖-康拉克地区的湖泊水域景观格局变化自1970s-2000年主要受车尔臣河径流量年际变化的控制,而21世纪以来则主要受塔里木河下游应急生态输水工程措施的影响.
Since the Lower Che’erchen River was rerouted in 1989, a number of small lakes formed to the north of the riverway, which greatly changed the pattern of waters in the Taitama Lake-Conlakur region. The Taitama Lake, which dried up for more than 30 years, Starting from the implementation of the emergency ecological water conveyance project in the lower reaches of the Tarim River, a large area of water started to form and the area of the water area was in an expanding trend. After the completion of the diversion of the Che’erchen River in 2002, the lake pattern in the Kanglak area basically formed while the waters in the Taitama Lake area Continue to change dramatically.This paper carries out various quantitative analyzes on the basis of 102 remote sensing images from 1972 to 2012 and their related auxiliary data to describe the process of waters changes in the Tai Tema Lake and Kanglake area in detail and sum up the trend of changes in an attempt to find out the changes The dominant factor.The author thinks that the change of lake landscape pattern in Tai Tema Lake-Kanglake area has been the control of the annual variation of the main driving factors in 1970s-2000, but the 21st century is mainly controlled by the emergency ecology in the lower reaches of the Tarim River Impact of water conveyance engineering measures.