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色林错面积时空变化遥感监测

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根据1976-2020年Landsat卫星遥感数据,通过NDWI和最大类间方差法构建该区域44年湖泊面积数据集,并结合流域周边的气象站资料、流域冰川等辅助数据对色林错湖面变化原因进行综合分析.结果表明:1976-2020年色林错面积增长752.33km2,共经历4个阶段:轻微增长(1976-1991年)、略微下降(1992-1997年)、急剧扩张(1998-2005年)和缓慢增长(2006-2020年).综合分析表明:气候要素是引起色林错湖泊面积变化的因素之一,而非关键因素,多种因素的结合促使色林错湖泊面积逐渐扩大.
Remote Sensing Monitoring of Spatial-temporal Changes in Siling Co Area
This paper constructs a 44-year lake area dataset in this region based on Landsat satellite data from 1976 to 2020 by NDWI and maximum inter-class variance method,and comprehensive analyzes the reasons for the changes of Siling Co lake surface by combining the meteorological station data around the basin,glaciers in the basin and other auxiliary data.The results show that the area of Siling Co grew by 752.33 km2 from 1976 to 2020,experiencing four stages:slight growth(1976-1991),slight decline(1992-1997),sharp expansion(1998-2005)and slow growth(2006-2020).Comprehensive analysis shows that the climate element is one of the factors causing the change of Siling Co lake area,rather than a key factor,and the combination of various factors contributes to the gradual expansion of Siling Co lake area.

Siling Coarea changeremote sensingclimate change

赖帆、赖百炼

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西安培华学院,陕西西安 710199

中煤航测遥感集团,陕西西安 710199

色林错 面积变化 遥感 气候变化

西藏那曲市林草局科研项目

2024

中国煤炭地质
中国煤炭地质总局

中国煤炭地质

CSTPCD
影响因子:0.652
ISSN:1674-1803
年,卷(期):2024.36(5)
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