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Monitoring of Moraine-Dammed Lakes: A Remote Sensing-Based Study in the Western Himalaya


Affiliations
1 Space Applications Centre (ISRO), Ahmedabad 380 015, India
2 M. G. Science Institute, Ahmedabad 380 009, India
 

Monitoring of lakes in glaciated terrain in the Himalayan region has been recognized as one of the priority areas especially after the Kedarnath disaster. Among all types of glacial lakes, moraine dammed lakes (MDLs) are the most important from disaster point of view. Remote sensing plays a significant role in view of availability of unbiased repeated data on the expansion or contraction of MDLs located in rugged terrains of the Himalaya. Monitoring of two MDLs, associated with Katkar and Gepang-gath glaciers in Zanskar and Chandra sub-basins respectively was done using satellite images of 1965, 1976, 1989, 2001, 2006-07, 2012 and 2014. Survey of India (SOI) topographical maps of 1962 were also referred to monitor the respective glaciers lakes. SOI maps show the presence of only one lake associated with Gepang-gath glacier. Areal extent of the MDLs had increased from 21 to 57 ha between 1965 and 2014, and from 27 to 80 ha between 1962 and 2014 for the Katkar and Gepang-gath glaciers respectively. Increase in peak discharge of the two lakes was also estimated using different empirical models in case of outbursts of these lakes. The lake outburst probability for both these lakes was found to be very low (less than 1%), however, possibility of outburst of lakes due to natural calamity like cloud burst, landslide or earthquake cannot be ignored. The rate of retreat of these two glaciers was observed to be high due to the presence of MDLs in comparison to surrounding glaciers in the valley.

Keywords

Glacier, Moraine Dammed Lake, Peak Discharge, Retreat.
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  • Kulkarni, A. V., Bahuguna, I. M., Rathore, B. P., Singh, S. K., Randhawa, S. S., Sood, R. K. and Dhar, S., Glacial retreat in Himalaya using Indian remote sensing satellite data. Curr. Sci., 2007, 92(1), 69–74.

  • Kulkarni, A. V., Rathore, B. P., Singh, S. K. and Bahuguna, I. M., Understanding changes in the Himalayan cryosphere using remote sensing technique. IJRS, 2011, 32(3), 601–615.

  • Brahmbhatt, Rupal, M., Bahuguna, I. M., Rathore, B. P., Kulkarni, A. V., Nainwal, H. C., Shah, R. D. and Ajai, A comparative study of deglaciation in two neighbouring basins (Warwan and Bhut) of Western Himalaya. Curr. Sci., 2012, 103(3), 298–304.

  • Bahuguna, I. M. et al., Are the Himalayan glaciers retreating? Curr. Sci., 2014, 106(7), 1008–1013.

  • Tweed, F. S. and Russell, A. J., Controls on the formation and sudden drainage of glacier-impounded lakes: implications for jokulhlaup characteristics. Prog. Phys. Geogr., 1999, 23, 79–110.

  • Clague, J. J. and Evans, S. G., A review of catastrophic drainage of moraine dammed lakes in British Columbia. Quaternary Sci. Rev., 2000, 19, 1763–1783.

  • Benn, D. I. and Evans, D. J. A., Glaciers and Glaciation, Hodder Education, London, 2010, p. 802; ISBN 978-0-340-90579-1.

  • Yamada, T., Glacier lake and its outburst flood in the Nepal Himalaya. Monograph no. 1, Data Center for Glacier Research, Japanese Society of Snow and Ice, Tokyo, 1998, p. 96.

  • Iturrizage, L., New observations on present and prehistorical glacier dammed lakes in the Shimshal valley (Karakoram mountains). J. Asian Earth Sci., 2005, 25, 545–555.

  • Benn, D. I., Wisemen, S. and Hands, K., Growth and drainage of supraglacial lakes on debris-mantled Ngozumpa glacier, Khumbu Himal, Nepal. J. Glaciol., 2001, 47, 625–638.

  • Hambrey, M. J., Quincey, D. J., Glasser, N. F., Reynolds, J. M., Richardson, S. J. and Clemments, S., Sedimentological, geomorphological and dynamic context of debris mantled glaciers, Mount Everest (Sagarmatha) region, Nepal. Quaternary Sci. Rev., 2008, 27, 2361–2389.

  • Sharma, A. K., Singh, S. K., Kulkarni, A. V. and Ajai, Glacier inventory in Indus, Ganga and Brahmputra basins of the Himalaya. Natl. Acad. Sci. Lett., 2013; doi:10.1007/s40009-013-0167-6.

  • Sakai, A., Takeuchi, N., Fujita, K. and Nekawo, M., Role of Supra-Glacial Ponds in the Ablation Process of a Debris Covered Glacier in the Nepal Himalaya, IAHS Publication, Washington, USA, 2000, vol. 264, pp. 53–61.

  • Komori, J., Recent expansions of glacial lakes in the Bhutan Himalayas. Quaternary Int., 2008, 184, 177–186.

  • Kulkarni, A. V., Dhar, S., Rathore, B. P., Govindharaj, K. and Kalia, R., Recession of Samudra Tapu glacier, Chandra River basin, Himachal Pradesh. J. ISRS, 2006, 34(1), 39–46.

  • Randhawa, S. S., Sood, R. K., Rathore, B. P. and Kulkarni, A. V., Moraine dammed lakes study in the Chenab and Satluj river basins using IRS data. J. ISRS, 2005, 33(2), 285–290.

  • Dhar, S., Kulkarni, A. V., Rathore, B. P. and Kalia, R., Reconstruction of the moraine dammed lake, based on field evidences and paleohistory, Samudra tapu glacier, Chandra basin, Himachal Pradesh. J. ISRS, 2009, 38, 133–141.

  • Govindharaj, K. B., Kumar, K. V. and Remya, S. N., Remote sensing based inventory of glacial lakes in Sikkim Himalaya: semiautomated approach using satellite data. Geomatics Nat. Hazards Risk, 2012; doi:10.1080/19475705.2012.707153.

  • Basnett, S., Kulkarni, A. V. and Bolch, T., The influence of debris cover and glacial lakes on the recession of glaciers in Sikkim Himalaya, India. J. Glaciol., 2013, 59(218), 1–12.

  • Bahuguna, I. M., Geomatics in early assessment of Himalayan lakes outburst hazards. Newsl. ISG, 2013, 19(2), 57–64.

  • Deslognes, J. R., Jones, D. P. and Kiker, K. E., Estimation of peak discharge from drainage of ice dammed Ape lake, British Columbia. Can. J. Glaciol., 1989, 35, 349–354.

  • Carey, M., Disasters, development and glacial lake control in twentieth-century Peru. In Mountains Sources of Water, Sources of Knowledge. Advances in Global Change Research (ed. Wiegandt, E.), Springer, the Netherlands, 2008, vol. 31, pp. 181–196.

  • Clarke, G. K. C. and Mathews, W. H., Estimation of magnitude of glacier outburst floods from Dojeck, Yukon Territory, Canada. Can. J. Earth Sci., 1981, 18, 1452–1463.

  • Gansser, A., Geology of the Bhutan Himalaya. Mem. Soc. Sci. Nat., 1983, 149–154.

  • Mason, K., Indus floods and Shyok glaciers. Himalayan J., 1929, 1, 10–29.

  • Bajracharya, R. S., Mool, P. K. and Shrestha, B. R., The impact of global warming on the glaciers of the Himalaya. In Proceedings of the International Symposium on Geo-disasters, Infrastructure Management and Protection of World Heritage Sites, Nepal Engineering College, Ehime College and National Society for Earthquake Technology, Nepal, 25–26 November 2006, pp. 231–242.

  • Fushimi, H., Ikegani, K., Higuchi, K. and Shankar, K., Nepal Case Study: Catastrophic Floods, Techniques for Prediction of Runoff from Glacierised Areas, IASH, Publ. No. 149, 1985, pp. 125–130.

  • Sangewar, C. V., Srivastava, D. and Singh, R. K., Reservoir within the Shaune Garang glacier, district Kinnaur, Himachal Pradesh. In Proceedings of the Symposium on Snow, Ice and Glaciers: A Himalayan Perspective, Abstr., Geological Survey of India, 1999, pp. 39–40.

  • Shrestha, B. B. and Nakagawa, H., Assessment of potential outburst floods from the Tsho Rolpa glacial lake in Nepal. Nat. Hazards, 2014, 71(1), 913–936.

  • Dobhal, D. P., Gupta, A. K., Mehta, M. and Khandewal, D. D., Kedarnath disaster: facts and plausible causes. Curr. Sci., 2013, 105(2), 171–174.

  • Akiko, S., Glacial lakes in the Himalayas: a review on formation and expansion processes. Global Environ. Res., 2012, 16, 23–30.

  • Clague, J. J. and Mathews, W. H., The magnitude of jokulaphs. J. Glaciol., 1973, 12, 501–504.

  • Aster GDEM team, Aster digital Global Digital Elevation model version 2 – summary of validations result. GDEM2, validation report final, http://www.ersdac or jp/GDEM/ver2validation/ summary, 2011 (accessed on 20 April 2012).

  • McKillop, R. J. and Clauge, J., Statitical remote sensing based approach for estimating the probability of catastishi drainage from moraine dammed lakes in southwestern British Columbia. Global Planet. Change, 2009, 56, 153–171.

  • Bhambri, R. and Bolch, T., Glacier mapping: a review with special reference to the Indian Himalayas. Prog. Phys. Geogr., 2009, 33, 672–704.

  • Kamp, U., Byrne, M. and Bolch, T., Glacier fluctuations between 1975 and 2008 in the Greater Himalayan Range of Southern Ladakh. J. Mt. Sci., 2011, 8, 374–389.

  • Kulkarni, A. V. and Karyakarte, Y., Observed changes in Himalayan glaciers. Curr. Sci., 2014, 106(2), 237–244.

  • Huggel, C., Kääb, A., Haeberli, W., Teysseire, P. and Paul, F., Remote sensing based assessment of hazards from glacier lake outbursts: a case study in the Swiss Alps. Can. Geotech. J., 2002, 39, 316–330.

  • O’Connor, J. E., Hardison, J. H. and Costa, J. E., Debris flows from failures of neoglacial-age moraine dams in the Three Sisters and Mount Jefferson wilderness areas, Oregon. US Geol. Surv. Prof. Pap., 2001, 1606, 93.

  • Xiaojun, Yao, Shiyin, Liu, Meiping, Sun, Junfenj, Wei, Wanqin, Guo, Volume calculation and analysis of the changes in morainedammed lakes in the North Himalaya: a case study of Longbasaba lake. J. Glaciol., 2012, 58(210), 753–760.

  • Costa, J. E. and Schuster, R. L., The formation and failure of natural dams. Geol. Soc. Am. Bull., 1988, 100, 1054–1068.

  • Costa, J. E., Rheologic, geomorphic, and sedimentologic differentiation of water floods, hyper-concentrated flows, and debris flows. In Flood Geomorphology (eds Baker, V. R., Kochel, R. C. and Patton, P. C.), John Wiley, New York, 1988, pp. 113–122.

  • Sangewar, C. V. and Kulkarni, A. V., Observational studies of the recent past. In Report of the Study Group on Himalayan glaciers prepared for the Office of the Principal Scientific Adviser to the Government of India, PSA/2011/2, 25-76, 2011.

  • Hall, D. K. et al., Consideration of the errors inherent in mapping historical glacier positions in Austria from the ground and space (1893–2001). Remote Sensing Environ., 2003, 86(4), 566–577.

  • Wang, Y., Hou, S. and Liu, Y., Glacier changes in the Karlik Shan, eastern Tien Shan, during 1971/72–2001/02. Ann. Glaciol., 2009, 50(53), 39–45.

  • Michael, P. and John, W., Jensen, Calculating area and volume of ponds and tanks. SRAC, USDA, Mississippi, Publication no. 103, 1991, pp. 1–7.


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  • Monitoring of Moraine-Dammed Lakes: A Remote Sensing-Based Study in the Western Himalaya

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Authors

B. P. Rathore
Space Applications Centre (ISRO), Ahmedabad 380 015, India
S. K. Singh
Space Applications Centre (ISRO), Ahmedabad 380 015, India
Rupal Brahmbhatt
M. G. Science Institute, Ahmedabad 380 009, India
I. M. Bahuguna
Space Applications Centre (ISRO), Ahmedabad 380 015, India
A. S. Rajawat
Space Applications Centre (ISRO), Ahmedabad 380 015, India
Ajai
Space Applications Centre (ISRO), Ahmedabad 380 015, India

Abstract


Monitoring of lakes in glaciated terrain in the Himalayan region has been recognized as one of the priority areas especially after the Kedarnath disaster. Among all types of glacial lakes, moraine dammed lakes (MDLs) are the most important from disaster point of view. Remote sensing plays a significant role in view of availability of unbiased repeated data on the expansion or contraction of MDLs located in rugged terrains of the Himalaya. Monitoring of two MDLs, associated with Katkar and Gepang-gath glaciers in Zanskar and Chandra sub-basins respectively was done using satellite images of 1965, 1976, 1989, 2001, 2006-07, 2012 and 2014. Survey of India (SOI) topographical maps of 1962 were also referred to monitor the respective glaciers lakes. SOI maps show the presence of only one lake associated with Gepang-gath glacier. Areal extent of the MDLs had increased from 21 to 57 ha between 1965 and 2014, and from 27 to 80 ha between 1962 and 2014 for the Katkar and Gepang-gath glaciers respectively. Increase in peak discharge of the two lakes was also estimated using different empirical models in case of outbursts of these lakes. The lake outburst probability for both these lakes was found to be very low (less than 1%), however, possibility of outburst of lakes due to natural calamity like cloud burst, landslide or earthquake cannot be ignored. The rate of retreat of these two glaciers was observed to be high due to the presence of MDLs in comparison to surrounding glaciers in the valley.

Keywords


Glacier, Moraine Dammed Lake, Peak Discharge, Retreat.

References





DOI: https://doi.org/10.18520/cs%2Fv109%2Fi10%2F1843-1849