Impact of Climate Change in Kalabaland Glacier from 2000 to 2013

S. Rahul Singh, R. Dhir
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Abstract

Glaciers are the coolers of the planet earth and the lifeline of many of the world’s major rivers. They contain about 75% of the Earth’s fresh water and are a source of major rivers. The interaction between glaciers and climate represents a particularly sensitive approach. On the global scale, air temperature is considered to be the most important factor reflecting glacier retreat, but this has not been demonstrated for tropical glaciers. Mass balance studies of glaciers indicate that the contributions of all mountain glaciers to rising sea level during the last century to be 0.2 to 0.4 mm/yr. Global mean temperature has risen by just over 0.60 C over the last century with accelerated warming in the last 10-15 years. The major impact will be on the world’s water resources. Many climatologists believe that the decline in mountain glaciers is one of the first observable signs of the human induced global warming.
2000 - 2013年气候变化对Kalabaland冰川的影响
冰川是地球的冷却器,也是世界上许多主要河流的生命线。它们含有地球上75%的淡水,是主要河流的源头。冰川和气候之间的相互作用是一种特别敏感的方法。在全球范围内,气温被认为是反映冰川退缩的最重要因素,但这一点尚未在热带冰川中得到证实。冰川的物质平衡研究表明,在上个世纪,所有山地冰川对海平面上升的贡献为0.2至0.4毫米/年。在过去的一个世纪里,全球平均气温上升了0.60摄氏度多一点,在过去的10-15年里,气候变暖加速。主要影响将是世界水资源。许多气候学家认为,高山冰川的减少是人类引起的全球变暖的最早可观察到的迹象之一。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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