首页> 外文会议>2013 3rd International workshop on image and data fusion >MONITORING THE CHANGES OF LAKES IN THE SOURCE REGION OF THREE RIVERS WITH REMOTE SENSING DATA FROM 1976 TO 2009
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MONITORING THE CHANGES OF LAKES IN THE SOURCE REGION OF THREE RIVERS WITH REMOTE SENSING DATA FROM 1976 TO 2009

机译:利用1976年至2009年的遥感数据监测三河源区湖泊的变化。

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As the birthplace of Yangtze River, the Yellow River and Lancang Rive, Source Region of Three Rivers (SRTR) is an important resource for fresh water supplement in China.SRTR also has very obvious ecological function which forms ecological security barrier for China's Qinghai-Tibet plateau.The inland lakes here play an important role for the water cycle in the plateau.The monitoring results were extracted with TM data from 1976 to 2009.The results show that from 1976 to 2009 the lakes' area in SRTR dropped first and then expanded with 2000 as sector.The lakes area was 6778 km2 in 2009, about 1.90% of the whole region, and increased than 1976 by 133.15 kin2.Most of the large lakes above 80 kin2 have the same change trend.The expanded lakes increased in number gradually, while the changes in the amplitude and time characteristics were different.From 1976 to 2000, the number of new lakes increased while died lakes dropped; and from 2000 to 2009 it is just on the contrary.In the study the index of lake change trend (ILCT) was adopted to contrast lake atrophy condition.With ILCT 24.55 there is an expansion trend for the lakes in SRTR during the last 35 years.The lakes with ILCT's absolute value greater than 1 were those merged with or disconnected from surrounding smaller lakes.Here the precipitation and snow melt are main supplies for the lakes.The change of lakes' area has well correlated with precipitation, and weak correlated with temperature from 1976 to 2009.But from 2000 to 2009, there has a strong correlation with precipitation, temperature.All these show from the side that the precipitation and snow melt are important factors to influence the lakes' change.The lakes have the coordination function for the good ecological environment in the region.The conclusions from the study can provide references in response to climate change research and rational utilization of water resources in SRTR.
机译:作为长江,黄河和澜沧江的发源地,三河源区(SRTR)是中国重要的淡水补充资源.SRTR还具有非常明显的生态功能,为中国青藏高原形成了生态安全屏障。高原内陆湖泊在高原水循环中起着重要作用.1976年至2009年利用TM数据提取了监测结果,结果表明1976年至2009年SRTR的湖泊面积先下降后扩大以2000年为单位。2009年湖泊面积6778 km2,约占整个湖泊面积的1.90%,比1976年增加133.15 kin2。80 kin2以上的大湖泊的变化趋势相同。从1976年到2000年,新湖的数量增加而死湖的数量减少。而从2000年到2009年恰好相反。在研究中,采用了湖变化趋势指数(ILCT)来对比湖泊的萎缩状况。ILCT24.55反映了SRTR在过去35年中湖泊的扩展趋势。 ILCT绝对值大于1的湖泊是与周围较小湖泊合并或分离的湖泊,这里的降水和积雪是湖泊的主要供给源,湖泊面积的变化与降水密切相关,而与湖泊的弱相关从1976年到2009年的温度,但从2000年到2009年,与降水,温度有很强的相关性,所有这些都从侧面表明降水和融雪是影响湖泊变化的重要因素。湖泊具有协调功能研究结论为SRTR气候变化研究和水资源的合理利用提供了参考。

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