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1993—2016年喀喇昆仑山中部Shigar流域冰川物质平衡变化空间特征研究 被引量:3
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作者 王璐 王宁练 +2 位作者 李志杰 陈安安 夏玮静 《冰川冻土》 CSCD 北大核心 2021年第1期1-13,共13页
基于Landsat系列卫星遥感影像、SRTM DEM和TanDEM-X DEM对喀喇昆仑山中部Shigar流域不同类型冰川的面积变化、物质平衡进行了分析。结果表明:1993—2016年间Shigar流域内有25条跃动冰川(面积增加1.30km2),68条前进冰川(面积增加0.86km2)... 基于Landsat系列卫星遥感影像、SRTM DEM和TanDEM-X DEM对喀喇昆仑山中部Shigar流域不同类型冰川的面积变化、物质平衡进行了分析。结果表明:1993—2016年间Shigar流域内有25条跃动冰川(面积增加1.30km2),68条前进冰川(面积增加0.86km2),50条退缩冰川(面积减少3.48km2),376条稳定冰川(面积减少1.34km2)。跃动冰川的冰川长度和规模均集中在较大范围内,前进冰川的规模略高于退缩冰川,退缩冰川多为小规模冰川,特大规模冰川保持稳定状态;不同类型冰川的空间分布差异较大,且不同海拔带内水热组合条件不一致也影响冰川运动状态。2000—2013年间,流域内跃动冰川物质平衡为(+0.17±0.03)m w.e.·a^(-1),前进冰川物质平衡为(-0.01±0.03)m w.e.·a^(-1),退缩冰川物质平衡为(-0.22±0.03)m w.e.·a^(-1),稳定冰川物质平衡为(-0.01±0.03)m w.e.·a^(-1)。四类冰川表面高程变化随归一化冰川长度的变化模式以及不同海拔带内和不同坡度区间的冰川表面高程变化显示:跃动冰川主要特征是积累区物质积累量大;前进冰川上部物质积累并且向下运动推动冰川末端前进;退缩冰川消融区物质亏损量大使得冰川末端退缩。 展开更多
关键词 喀喇昆仑山 shigar流域 冰川 表面高程变化 物质平衡
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Remote Sensing Data Application to Monitor Snow Cover Variation and Hydrological Regime in a Poorly Gauged River Catchment—Northern Pakistan
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作者 Samreen Abdul Hakeem Muhammad Bilal +1 位作者 Arshid Pervez Adnan Ahmad Tahir 《International Journal of Geosciences》 2014年第1期27-37,共11页
Snow- and glacier-nourished river basins located in the Himalaya-Karakoram-Hindukush (HKH) ranges supply a significant amount of discharge in River Indus upstream Tarbela Dam. It is, hence, important to comprehend the... Snow- and glacier-nourished river basins located in the Himalaya-Karakoram-Hindukush (HKH) ranges supply a significant amount of discharge in River Indus upstream Tarbela Dam. It is, hence, important to comprehend the cryosphere variation and its relationship to the stream flow in these high-altitude river catchments. The MODIS remotely sensed database of snow products was chosen to examine the average annual snow and glacier cover (cryosphere) variations in the Shigar River basin (poorly gauged mountainous sub-catchment of the Indus River). Hydrological regime in the area was investigated through monthly database of observed stream fluxes and climate variables (precipitation and mean temperature) for the Shigar River catchment. Analysis indicated the usefulness of remote sensing techniques for estimation of the snow cover variation in the poorly or un-gauged high-elevation catchments of the HKH zone. Results also showed that Shigar River discharge was influenced mainly by the seasonal and annual snow cover area (SCA) variation and the temperature seasonality. Moreover, it is important to uncover such inter-relationship of stream flow, climate variables and snow cover in the poorly gauged high-altitude catchments of Karakoram region for better water resource management and accurate flood hazards predictions at Tarbela. 展开更多
关键词 shigar RIVER basin Satellite Remote Sensing MODIS SNOW Products Water RESOURCES Management ASTER-GDEM
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