首页> 外文期刊>Geomorphology >Inventory of rock glaciers in Himachal Himalaya, India using high-resolution Google Earth imagery
【24h】

Inventory of rock glaciers in Himachal Himalaya, India using high-resolution Google Earth imagery

机译:使用高分辨率谷歌地球图像,在印度喜喜马拉雅喜马拉雅山的岩石冰川库存

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

Little information about the number, spatial distribution, and characteristics of rock glaciers in Himachal Himalaya is available. This information is crucial to assess the hydrological contribution of permafrost regimes and to understand its response to changing climate. Employing high-resolution satellite data freely accessible through Google Earth, the first comprehensive rock glacier inventory of Himachal Himalaya is presented in this work. The inventory reports 516 rock glaciers in the study area corresponding to an estimated area of 353 km(2) of which 59% have glacier origin and 41% have talus origin. The frontal elevation of the lowest rock glacier in the Himachal Himalaya is 3052 m above sea level which was significantly low, whereas the highest rock glacier occurs at 5503 m above sea level. The mean minimum elevation of rock glaciers was 4484 m above sea level and the maximum was 4900 m above sea level. The majority of the rock glaciers have a northerly aspect (N, NE, NW) followed by westerly aspect signifying that slopes with lower potential incoming solar radiation favour the formation of rock glaciers. The mean annual surface temperature of the rock glaciers derived from Moderate Resolution Imaging Spectroradiometer (MODIS) Land surface temperature (1ST) product (MOD11B3) was -1.5 degrees C, with glacier-derived rock glaciers having colder surfaces than talus-derived rock glaciers. The topographical and climatological parameters greatly influenced the formation and development of rock glaciers. (C) 2019 Elsevier B.V. All rights reserved.
机译:有关喜马拉雅山岩石冰川岩石冰川的数量,空间分布和特征的少量信息。这些信息对于评估多年冻土制度的水文贡献并了解其对变化气候的反应至关重要。采用高分辨率卫星数据通过谷歌地球自由进入,这项工作中的第一个全面的岩石冰川库存呈现出来的喜马拉雅山。库存报告516研究区中的岩石冰川对应于353 km(2)的估计面积59%具有冰川起源,41%具有塔卢斯来源。喜马拉雅喜马拉雅山上最低岩石冰川的正面高度为海拔3052米,岩石冰川最高的冰川发生在5503米以上海拔5503米。岩石冰川的平均最小升高为海拔4484米,海拔最高4900米。大多数岩石冰川具有北方的方面(N,NE,NW),然后是西方方面,表示具有较低潜在的传入的太阳辐射的斜坡倾向于岩石冰川的形成。源自中等分辨率成像分光镜(MODIS)陆地温度(1ST)产品(MOD11B3)的岩石冰川的平均年表面温度为-1.5℃,冰川衍生的岩石冰川具有比缩略图的岩石冰川更冷的表面。地形和气候学参数极大地影响了岩石冰川的形成和发展。 (c)2019 Elsevier B.v.保留所有权利。

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