Morpho-metric Characteristics of Glaciers in the Indian Himalayas

Statistical analyses of the glacio-morpho metric parameters show a spatial variation across Himalaya. Glacier density varies across Himalaya: it is maximum in the Sutlej and Tista basin and moderate in the Jhelum and Bhagirathi basin, while least density area is in Arunachal Pradesh basin. Most of the glaciers are simple type while some glaciers are big in size and composite in nature. The single biggest glacier contributes about 30% of the total glacier cover in the respective basins. Length and width change from west to east and consequently the elongation, relief ratio and relief area gradient. These indices suggest that the west glaciers are stream type, while eastern glaciers are patch type and occupied in high relief region.
Health of glaciers can be inferred using Accumulation Area Ratio (AAR) and the average AAR value of the Indian glaciers is 0.48; a state of negative mass balance. A comparative analysis of glaciers AAR shows that the glaciers having zero AAR constitute about 34% of total glaciers, while glaciers having near 100 AAR constitute about 9% of total number of the glaciers. Correlation matrix between various glacio-morpho metric parameters suggests that the AAR is closely related to accumulation area, length, mean elevation and area
The accumulation zone is gentler slope area of the glaciers and a slight shift in zero isotherms on the accumulation surface will result in quick shrinkage in accumulation area. It will further contribute to more negative mass balance and development of supraglacial and moraine dammed lake in glaciated region. Present study clearly indicates the high susceptibility of the glacier shrinking in Indian Himalaya in the present climatic change regime.
Ahmad, N. and S. Rais (1999). Himalayan glacier. APH Publishing Corporation, New Delhi, 150 pp.
Benn, D. and L.A. Owen (1998). The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciations: Review and speculative discussion. Journal of the Geological Society, 155: 353-363.
Cotton, C.A. (1942). Climatic accidents in landscape laking. John Wiley & Sons, New York, 354 pp.
Dhobal, D.P. (1995). Morphology and glacier dynamics studies in monsoon arid transition zone: An example from Chhota Shigri glacier, Himachal Himalaya, India. Current Science, 68 (9): 936.
Dhobal, D.P and J.T. Gergon (1996). Mass balance study of Dokriani glacier, Garhwal Himalaya. Technical report, Multi-disciplinary Multi-Institutional glaciological expedition to Dokriani glacier, Garhwal Himalaya. DST Report, 1996, Glaciology Division, 260 pp.
Doornkamp, J.C. and C.A.M. King (1971). Numerical analysis in geomorphology. Edward Arnold London, pp. 1-181.
Flint, R.F. (1963). Glacial Pleistocene Geology. John Wiley & Sons, New York, 553 p.
Hastenrath, S. (1995). Glacier Recession on Mount Kenya in context of Global tropics. Bull Inst. Fr. Etudes andines, 24 (3): 633-638.
Inoue, J. (1977). Mass budget of Khumbo glacier. Seppyo. Special issue, 39: 15-19.
Kaser, G. (1995). Some notes on the behaviour of tropical glaciers. Bull Inst. Fr. Etudes andines, 24 (3): 671-681.
Kaul, M.M. (1995). Inventory of the Himalayan Glacier. In: M.K. Special Publication No. 34. Geological Survey of India, pp. 165.
Kulkarni, A.V. (1992). Mass Balance of Himalayan glacier using AAR and ELA methods. J. of Glaciol., 38 (128): 101.
Mukherjee, B.P. and C.V. Sangewar (1995). Correlation of Accumulation Area Ratio and ELA with mass balance of Gara, Gor Garang and Shaune Garang glaciers of Himachal Pradesh. Proc. Symp., NW Himalaya and foredeep. Feb. 1995. Geol. Surv. India. Sp. Pub., 21 (2): 303.
Muller, F. (1978). Instruction for compilation and assemblage of data for a world glacier inventory. Dept. of Geography, Swiss Federal Institute of Technology, Zurich, Paterson, W.S.B., 1981, The physics of glaciers. Pergmon Press, second edition, 42-57.
Muller, F., Caflish, T. and G. Muller (1977). Instruction for compilation and assemblage of data for a world glacier inventory. Dept. of Geography, Swiss Federal Institute of Technology, Zurich, 30 p.
Naithani, A.K., Nainwal, H.C., Sati, K.K. and C. Prasad (2001). Geomorphological evidences of retreat of Gangotri glacier and its characteristics. Curr. Sci., 80: 87-94.
Owen, L.A., Derbyshire, E. and M. Fort (1998). The Quaternary glacial History of the Himalaya. Quaternary Proceeding, 6: 21-142.
Owen, L.A., Finkle, R.C., Caffee, M.W. and L. Gualtieri (2002). Timing of multiple late Quaternary glaciations in the Hunza valley, Karokoram Mountain, Northern Pakistan: Defined by cosmogenic radionuclide dating moraines. Geological Society of America Bulletin, 114 (5): 593-604.
Prasad, C. and A.K. Naithani (2003). Glacier Morphometry: A case study of Gangotri Group of glaciers. Garhwal Himalaya, India. Journal of the Geological Society of India, 61: 325-334.
Richard, B.W.M., Ben, D.I., Owen, L.A. and J.Q. Spencer (2000). Timing of late Quaternary glaciations south of Mount Everest in the Khumbu Himal, Nepal. Geological Society of America Bulletin, 112 (10): 21-32.
Thompson, L.G., Mosley–Thompson, E., Davis, M.E., Lin, P.N., Henderson, K.A., Cole-Dai, J., Bolzon, J.F. and K.B. Liu (1995). Last Glacial Stage and Holocene tropical ice core records from Huascaran. Peru. Science, 269: 46-50.
Wagnon, P., Ribestein, P., Kaser, G. and P. Berton (1999). Climate variability energy balance and runoff on a tropical glacier. Global Planetary Changes, 22: 49-58.
Weismen, V. (1959). Die Hentige Verglets#herung and Schneegrenze im Hoch¡sien, mit Hinweisen auf die Ve²gletsherung der letzen Eisziet. (Contemp. Glaciation and snowloaen in High Asia). Akad Wissen s#chaften und der litertur in Mani2. Abhandlungne der Math-Naturdwissen schaftlichen Klassee, Ja$arg no. 14, pp. 1150-1407.
Zongtai, W. and Y. Huian (1992). Characteristics of the distribution of glaciers in China. Ann. of Glaciol., 16: 17-20.