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COMPARISON OF ENERGY BALANCE ON GANGOTRI AND CHHOTA SHIGRI GLACIERS

机译:节能与Chhota shigri冰川能量平衡的比较

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Surface energy balance of a glacier governs the physical processes taking place at the surface-atmosphere interface and connects ice ablation/accumulation to climate variability. To understand the response of Himalayan glaciers to climatic variability, a study was taken to formulate energy balance equation on two of the Indian Himalayan glaciers, one each from Indus and Ganga basins, which have different climatic and physiographic conditions. Study was carried out over Gangotri glacier (Ganga basin) and Chhota Shigri(CS) glacier from Chandra sub-basin (Indus basin). Gangotri glacier is one of the largest glaciers in the central Himalaya located in Uttarkashi District, Uttarakhand, India. Chhota Shigri glacier of Chandra sub-basin lies in Lahaul and Spiti valley of Himachal Pradesh. Energy balance components have been computed using inputs derived from satellite data, AWS (Automatic Weather Station) data and field measurements. Different components of energy balance computed are net radiation (includes net shortwave and net longwave radiation), sensible heat flux and latent heat flux. In this study comparison has been made for each of the above energy balance components as well as total energy for the above glaciers for the months of November and December, 2011. It is observed that net radiation in Gangotri glacier is higher by approximately 43% in comparison to Chhota Shigri glacier; Sensible heat flux is lesser by 77%; Latent heat flux is higher by 66% in the month of November 2011. Comparison in the month of December shows that net radiation in Gangotri glacier is higher by approximately 22% from Chhota Shigri glacier; Sensible heat flux is lesser by 90%; Latent heat flux is higher by 3%. Total energy received at the glacier surface and contributes for melting is estimated to be around 32% higher in Gangotri than Chhota Shigri glacier in November, 2011 and 1.25% higher in December, 2011. The overall results contribute towards higher melting rate in November and December, 2011 in Gangotri than Chhota Shigri glacier.
机译:冰川的表面能量平衡控制表面大气界面处发生的物理过程,并将冰烧蚀/积累与气候变异性连接。要了解喜马拉雅冰川对气候变异性的响应,采取了一项研究,以制定两个印度喜马拉雅冰川的能量平衡方程,每个人都来自indus和ganga盆地,其具有不同的气候和地理学条件。从Chandra子盆地(印度盆地)的甘蓝冰川(Ganga Basin)和Chhota Shigri(CS)冰川进行了研究。 Gangotri Glacier是喜马拉雅市中心最大的冰川之一,位于印度Uttarkashi区埃略齐齐区。 Chandra Shigri的Chhota Shigri冰川位于马偕尔邦的拉拉和斯皮蒂谷。已经使用从卫星数据,AWS(自动气象站)数据和现场测量的输入来计算能量平衡组件。计算的能量平衡的不同组件是净辐射(包括净短波和净龙波辐射),明智的热通量和潜热通量。在这项研究中,对于上述每个能量平衡组件以及上述冰川的总能量,已经为11月和12月的上述冰川的总能量进行了比较。观察到甘蓝冰川的净辐射较高约43%与Chhota Shigri冰川相比;明智的热通量较小为77%; 2011年11月潜伏的热量持续增长率较高66%。12月份的比较表明,甘蓝冰川的净辐射从Chhota Shigri冰川较高约22%;明智的热通量较小为90%;潜热通量较高3%。在冰川表面接收的总能量和融化的贡献估计在2011年11月的Chhota Shigri冰川比Chhota Shigri冰川高出32%。总成果11月和12月促进了较高的熔化率,2011年在甘蓝比Chhota Shigri冰川。

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