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12-14 September, 2011, Lucknow - Earth Science India

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National Conference on <strong>Science</strong> of Climate Change and <strong>Earth</strong>’s Sustainability: Issues and Challenges ‘A Scientist-People Partnership’<br />

<strong>12</strong>-<strong>14</strong> <strong>September</strong>, <strong>2011</strong>, <strong>Lucknow</strong><br />

approx. 0.285 km between 1962 and 1990. Then after glacier retreated to the tune of<br />

0.230 km upto 1997. Subsequently, the southern limb experiences surge during 1997 to<br />

2001 by 0.670 km and during 2001 to 2008 it again shows retreat.<br />

Chong Kumdan Glacier<br />

This glacier has three prominent limbs, the northern, central and southern. The<br />

1975 topographical sheets demonstrate that all the three limbs are merging together to<br />

form a single snout. The 1990 satellite data shows that the northern and the central<br />

limbs still remain merged together while the southern limb shows a slight retreat. The<br />

relative retreat of the northern, central and southern limbs between different years have<br />

been monitored in the present investigation.<br />

The Northern limb has demonstrated alternating advance and retreat in subsequent<br />

years upto the year 2004. Between 1990 and 1992 this shows a retreat of approx. 50 m.<br />

while between 1992 and 1996 this limb advances by approx. 300 m. Subsequently, this<br />

again shows a retreat of 300 m. between 1996 and 1997. This surge and the retreat<br />

phenomena is continuous until 2004, where after between 2004 and 2005 this northern<br />

limb shows an abrupt advance of almost 1100 m. In subsequent years this frontal part of<br />

the northern limb gradually retreats back until 2009. On the whole, the northern limb<br />

shows an overall surge of approximately 2278 m. between 1997 and 2009.<br />

The Central limb show pre-dominantly retreat phenomena upto 2001 and then<br />

after there is a continuous surge in the frontal part of this limb. Between 2005 and 2006<br />

this frontal part has advanced by almost 500 m. and then again between 2006 and 2007,<br />

this has further surged by another 450 m. This limb starts to recede back between 2008<br />

and 2009.<br />

The Southern limb also has a history of relative oscillations during the period of<br />

observation. This advances upto 1996 and then retreats back upto 1999. Between 1999<br />

and 2000 this again advances by almost 370 m. where after the frontal part against<br />

recedes back. Between 2003 and 2004 this again shows surge while between 2004-05<br />

and 2005-06 this again retreats back. From 2007 onwards this limb shows a continuous<br />

surge of approx. 400 m.<br />

The coalescence of northern and central limb of Chong Kumdan glacier has given<br />

rise to a very distinct medial moraine. The central limb pushes the northern limb upto<br />

1997 where after the trend changes and the northern limb starts surging ahead and<br />

pushing the central limb. This is clearly demonstrated by the shifting of the medial<br />

moraine by approx. 2200 m. over a period between 1997 and 2009.<br />

Kichik Kumdan Glacier<br />

This glacier has a northern limb and southern limb. The 1975 topographical data<br />

shows that both limbs merge together to form a single snout. The northern limb shows a<br />

marked retreat of 0.53 m during 1990 to 1997. The frontal lobe of the glacier shows<br />

interesting phenomena. The 1975 topographical sheet demonstrates that the frontal lobe<br />

is pushing the Shyok River to the left bank. Between 1975 and 1990 this frontal part has<br />

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