首页> 外文期刊>Zeitschrift fur Geomorphologie >Glacier changes in Upper Tons River basin, Garhwal Himalaya, Uttarakhand, India
【24h】

Glacier changes in Upper Tons River basin, Garhwal Himalaya, Uttarakhand, India

机译:印度北阿坎德邦加尔瓦尔·喜马拉雅山上特恩斯河流域的冰川变化

获取原文
获取原文并翻译 | 示例
       

摘要

We estimate the spatial changes in the Jaundhar, Jhajju and Tilku glaciers in the Tons River basin (Garhwal Himalaya) between 1962 and 2010 using Landsat Satellite data, topographic maps along with field surveys. We estimate the overall shrinking in the area of the glaciers to be ~ 3.6 km~2 (5.4% of total area) and ~ 1,709 m, ~ 800 m and ~ 700 m of frontal retreat (snout) with an average of 34.18, 15.38 and 13.46m a~(-1) for the Jaundhar, Tilku and Jhajju Glaciers respectively. However, frontal retreat rates are not uniform in all glaciers even under the same climatic domain. The Jaundhar Glacier (55 km~2) has been separated into two parts; North Jaundhar (40 km~2) and South Jaundhar (15 km~2) between 1975 and 1990. Study on these fragmented glaciers shows a continuous and unusual retreat of glaciers after 1990. Compared with the regional mean of glaciers retreat in the Uttarakhand Himalaya, the glaciers show heterogeneous retreat rates. This uncertainty may possibly be due to size, surface morphology and gradient of the individual glaciers and can be attributed to degeneration and rapid melting on the glaciers. Meteorological data available from this region show increasing summer temperature and less winter precipitation in last few decades. Further more studies on these glaciers will shed light on several factors influencing changes and retreat on the Himalayan glacier systems.
机译:我们使用Landsat卫星数据,地形图以及实地调查,估算了1962年至2010年Tons河盆地(Garhwal Himalaya)的Jaundhar,Jhajju和Tilku冰川的空间变化。我们估计冰川面积的总体收缩为〜3.6 km〜2(占总面积的5.4%)和〜1,709 m,〜800 m和〜700 m的正面退缩(snout),平均为34.18、15.38 Jaundhar,Tilku和Jhajju冰川分别为13.46ma〜(-1)。但是,即使在相同的气候范围内,所有冰川的额叶退缩率也不相同。 Jaundhar冰川(55 km〜2)已分为两部分。在1975年至1990年之间,北黄道(40 km〜2)和南黄道(15 km〜2)。对这些破碎的冰川的研究表明,1990年以后冰川连续而不同寻常地后退。与北阿坎德邦喜马拉雅山的冰川后退区域平均值相比,冰川显示出不同的退缩率。这种不确定性可能是由于单个冰川的大小,表面形态和梯度造成的,并且可以归因于冰川的退化和快速融化。从该地区获得的气象数据显示,过去几十年来夏季气温升高,冬季降水减少。对这些冰川的进一步研究将揭示影响喜马拉雅冰川系统变化和后退的几个因素。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号