首页|基于遥感的柴达木盆地湖泊面积变化与气候响应分析

基于遥感的柴达木盆地湖泊面积变化与气候响应分析

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利用MODIS09卫星遥感数据,对比6种水体指数法(NDWI、MNDWI、EWI、NWI、DLWI、MDLWI)的湖泊提取结果,最终采用归一化水体指数法NDWI对柴达木盆地2001-2014年连续14年的湖泊面积进行解译.结合当地气象资料和冰川面积的变化情况,对影响区内湖泊面积变化的因素进行了分析.结果表明,2001-2014年柴达木盆地的湖泊呈先增加后减少的趋势变化.区内<1 km2的湖泊个数最多,10~100km2和>100 km2等级的湖泊面积所占比例最大,平均分别占总面积的36%和58%.区内湖泊主要分布在海拔低于3 000m的中部平原区.近14年研究区气温整体较高,降水与湖泊面积变化情况一致,蒸发量缓慢减少.区内冰川面积和储量整体呈缓慢减少的趋势,冰川面积与湖泊面积呈显著负相关关系.降水增加、蒸发减少和冰川消融是影响区内湖泊面积变化的根本因素.
Response of lake area variation to climate change in Qaidam Basin based on remote sensing
Based on MODIS09 data,the lake areas were extracted from 2001 to 2014 in Qaidam Basin using Normalized Difference Water Index (NDWI) after we compared the results of 6 methods of water index.Combined with meteorological data and glaciers area variation,the impact factors of lake area change in Qaidam Basin were analyzed.The result shows that the lake area in Qaidam Basin increased first and then decreased.The number of lakes with area smaller than 1 km2 was the maximum.The lake area between 10 and 100 km2,and area with larger than 100 km2 occupied 36% and 58% of the total area,respectively;they occupied a large portion of the total lake area.Most lakes were located at plain area with elevation smaller than 3000 m.In the last 14 years,the air temperature of the study area was at a high level and precipitation in the basin changed consistent with lakes change while the evaporation decreased slowly.Overall,the glaciers area and reserves in Qaidam Basin decreased slowly,and there was negative correlation between the variation of lakes and glaciers area.The increase of precipitation and decrease of evaporation and glacier melt are fundamental factors for the lake area change.

MODIS dataNormalized Difference Water Index(NDWI)lakesglaciersQaidam Basin

魏善蓉、金晓媚、王凯霖、梁华

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中国地质大学(北京)水资源与环境学院,北京100083

MODIS数据 归一化差异水体指数(NDWI) 湖泊 冰川 柴达木盆地

国家自然科学基金

41372250

2017

地学前缘
中国地质大学(北京) 北京大学

地学前缘

CSTPCDCSCD北大核心EI
影响因子:2.431
ISSN:1005-2321
年,卷(期):2017.24(5)
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