青藏高原近25年来河流、湖泊的变迁及其影响因素

    Changes of rivers and lakes on the Qinghai-Tibet Plateau in the past 25 years and their influence factors

    • 摘要: 结合20世纪70年代中期的MSS图像和90年代末期的ETM+图像解译,对近25年来青藏高原河流、湖泊的分布现状及其变迁进行了分析。研究表明,青藏高原河流总体上变化不明显,部分地区外流水系个别河段略有摆动,内流水系少数河段发生改道、断流,入湖河流河口段发生延伸、退缩等变化。青藏高原多数天然湖泊变化较大,主要是部分湖泊面积缩小或扩大;少数湖泊解体或归并;有的已干涸的湖泊又重新汇水,有的湖泊则接近干涸。导致河流、湖泊演变的主要影响因素有气温变化、降水变化及冰川变化、气候雪线变化等。

       

      Abstract: The present status and changes of distribution of rivers and lakes on the Qinghai-Tibet Plateau in the past 25 years have been analyzed according to the interpretation of the MSS remote sensing images in the middle 1970s and the ETM+ images at the end of the 1990s. Study indicates that: in general there is no appreciable change of rivers on the Qinghai-Tibet Plateau; a few river stretches of exterior drainages in some areas fluctuate slightly and a few river stretches of interior drainages are diverted or run dry; the river-mouth stretches where rivers inflow into lake show extensional and recessional changes. Most natural lakes on the plateau change significantly, mainly manifested by the following aspects: some lakes are reduced or expanded in area, some lakes are disintegrated or merged, water are again collected in some dried-up, and some lakes are nearly dried-up. The main influence factors leading to the changes of rivers and lakes include air temperature change, precipitation change, glacier change and climatic snow line change.

       

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