Imja glacier The Imja glacier and Imja Tsho As a special focus of this study, we will analyse the development of the Imja glacier during the past 50 years. The Imja glacier is located at 27.54° N and 86.56° E in the Khumbu Himal (Look at figures 6 and 7). It originates on the western face of Kali Himal and is joined by the Lhotse Shar and Ambulapcha glaciers before it drains into the Imja Khola. The Imja Tsho is a glacial lake that appeared in the 1960’s and is still growing at the rate of about 10 m per year. This makes it a very unstable construction, and is a threat to the inhabitants downstream the Dingboche and Imja Khola valley, which is the most densely populated Sherpa valley in Nepal. About 28 million m3 of dammed water could flood the valley in the case of a flood outburst.
Additionally, with the launch of the first Earth surveying satellites in the 1960’s, optical imagery can now be used to detect changes in the glacier and the lake. Aerial photographs can also be used. With the launch of the first civilian satellites such as the Landsat Multispectral Scanner (MSS) in the 1970’s, a time-scheduled surveying instrument was born to map the Earth with 'fresh' data every 18 days. More of those instruments with higher spatial resolutions and higher repletion rates appeared during the 1980’s and 1990’s with the Landsat Thematic Mapper (TM) and Enhanced Thematic Mapper Plus (ETM+), among others.
Last update: 16 April 2013
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