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阿牙克库木湖动态变化及其对冰川消融的响应

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基于Landsat TM卫星遥感数据,应用水体指数法,对新疆祁漫塔格地区阿牙克库木湖的面积变化进行了研究,并分析其影响因素。结果表明:1989—2010年,湖泊面积呈明显增加趋势,增加量为294.9 km2,总体增长率为48.7%,其中2000—2006年湖泊面积增大最快;阿牙克库木湖的面积变化与气象因素密切相关,研究区气温和降水量在22 a间均呈上升趋势;湖泊变化还与冰川消融有关,祁漫塔格地区1989—2006年冰川面积退缩率为20.0%,2006—2011年冰川面积退缩率为7.2%,而1989—2006年、2006—2011年冰储量的减少率分别为26.0%和9.5%,与湖泊面积的增长趋势相吻合。
Dynamic Change of Ayakekumu Lake and Its Response to Glaciers Melting
The change of lake indicates the variation of climate and environment. Based on Landsat TM satellite data and New Water Index ( NWI) , this paper studied the areal change of Ayakekumu Lake and its impact factors in Qimantage area of Xinjiang Autonomous Region. The results show that the lake area is increased by 294.9 km2 from 1989 to 2010 and the increase rate is 48.7%. The fast increase period is from 2000 to 2006. The dynamic change of lake area is related with climate factors. Both air temperature and precipitation are increased during the 22 years. On the other hand, the areal change of lake is also related with glaciers melting. The glacier area decrease rate is 20%from 1989 to 2006. Similarly, the glacier area decrease rate is 7.2% from 2006 to 2011. The decrease rates of glacier reserves are 26.0% and 9.5% during the two periods of 1989 to 2006 and 2006 to 2011, respectively. This trend is coincidence with the increase of lake area.

water indexLandsat TM dataglacier meltingglacier reserveAyakekumu Lake

王松涛、金晓媚、高萌萌、柳王吉

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新疆地矿局 第二水文工程地质大队,新疆 昌吉831100

中国地质大学 水资源与环境学院,北京100083

水体指数法 Landsat TM数据 冰川消融 冰储量 阿牙克库木湖

国家自然科学基金资助项目

41372250

2016

人民黄河
水利部黄河水利委员会

人民黄河

CSTPCD北大核心
影响因子:0.494
ISSN:1000-1379
年,卷(期):2016.38(7)
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