3.9 Article

Spatio-temporal changes in the Machoi glacier Zanskar Himalaya India using geospatial technology

Journal

QUATERNARY SCIENCE ADVANCES
Volume 4, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.qsa.2021.100031

Keywords

Snout retreat; Glacier dynamics; Climate change; Zanskar Himalaya; Geospatial technology

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The study analyzed the temporal changes of the Machoi glacier in the Zanskar region of the north-western Himalaya, India from 1973 to 2018 using multi-temporal Landsat satellite data, revealing a consistent retreat with varying rates over the past 45 years. The glacier snout retreated an average of 563 meters, with different retreat rates in different time intervals, particularly showing a higher rate during 2010-2018, possibly influenced by climate change factors such as increased temperature and decreased solid precipitation.
We present the temporal changes of Machoi glacier, Zanskar region of the north-western Himalaya, India using multi-temporal Landsat satellite data from 1973 to 2018. The results suggest that the Machoi glacier has retreated consistently from last 45 years with an uneven retreat rate. The temporal fluctuations since 1973 AD reveal that the glacier snout has retreated similar to 563 m at an average of similar to 12.51 m yr(-1). However, the snout has retreated at variable rates during different time intervals e.g., 80 m (average of similar to 11.43 m yr(-1)) from 1973 to 1980 AD, 120 m (average of similar to 12.0 m yr(-1)) from 1980 to 1990 AD, 123 m (average of similar to 12.3 m yr(-1)) from 1990 to 2000 AD, 128 m (average of similar to 12.8 m yr(-1)) from 2000 to 2010 AD and 112 m (average of similar to 14 m yr(-1)) from 2010 to 2018AD. The highest rate of snout (similar to 14 m yr(-1)) retreat during 2010-2018 AD is linked to the changing climate in the region as observed from the meteorological data. The analysis of meteorological data suggests that during this period temperature as well as the liquid precipitation have increased due to global warming whereas the extent of solid precipitation has decreased which might be the possible causes of higher retreat of Machoi glacier.

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