首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Monitoring of great Himalayan glaciers in Patsio region, India using remote sensing and climatic observations.
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Monitoring of great Himalayan glaciers in Patsio region, India using remote sensing and climatic observations.

机译:使用遥感和气候观测资料监测印度Patsio地区的喜马拉雅大冰川。

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Three glaciers, namely Panchi-Nala, Zing-Zing-Bar and Baralacha-La in the Patsio region, Great Himalaya, India were monitored between 1971 and 2011 using satellite data. These glaciers were selected based on their terminus altitude, slope variations and debris cover. The Landsat, Corona, LISS-IV and Cartosat-1 satellite data were analysed to monitor variations in the area of glacier, terminus and annual snow line. Glacier outlines from the satellite imageries were generated using hybrid technique consisting of visual interpretation, band ratio, NDSII and thermal band (TM and ETM+) data. Glacier outline was also verified by GPS survey on Zing-Zing-Bar in 2011. The total loss in the area of a glacier was observed to be maximum (16.35+or-3.74%) for the smallest glacier, i.e. Baralacha-La glacier between 1971 and 2011. A maximum average retreat in glacier terminus of 22.5 ma-1 was observed for the Zing-Zing-Bar glacier, whereas for Panchi-Nala and Baralacha-La glaciers, the average retreat rate was observed to be 9.2 and 10 ma-1 respectively. An upward shift in Equilibrium Line Altitude was observed for all the glaciers between 1971 and 2011. The climate data collected at SASE meteorological station, Patsio (3800 m) between 1983 and 2011 suggests an increasing trend in the mean annual temperature and a decreasing winter precipitation. These observations support the effect of climate variability on spatial variation of glaciers in the Patsio region. Non-climatic factors such as size of the glacier, slope variation and debris cover were found to influence variable responses of different glaciers in the same climatic zone.
机译:1971年至2011年之间,使用卫星数据监测了印度大喜马拉雅山Patsio地区的三座冰川,分别是Panchi-Nala,Zing-Zing-Bar和Baralacha-La。这些冰川是根据其终点高度,坡度变化和碎屑覆盖率选择的。对Landsat,Corona,LISS-IV和Cartosat-1卫星数据进行了分析,以监测冰川,终点和年雪线面积的变化。卫星图像的冰川轮廓是使用混合技术生成的,该技术包括视觉解释,波段比,NDSII和热波段(TM和ETM +)数据。冰川轮廓在2011年通过Zing-Zing-Bar的GPS调查也得到了验证。对于最小的冰川(即巴拉拉恰-拉格冰川),冰川面积的总损失最大(16.35+或-3.74%)。 1971年和2011年。Zing-Zing-Bar冰川的冰川终站最大平均退缩率为22.5 ma -1 ,而Panchi-Nala和Baralacha-La冰川的平均退缩率为分别为9.2和10 ma -1 。在1971年至2011年之间,所有冰川的平衡线高度都出现了上升趋势。在1983年至2011年之间,SASE气象站Patsio(3800 m)收集的气候数据表明,年平均气温呈上升趋势,而冬季降水减少。这些观察结果支持了气候变化对帕特西奥地区冰川空间变化的影响。发现非气候因素,例如冰川的大小,坡度变化和碎屑覆盖率,会影响同一气候区内不同冰川的变量响应。

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