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Chapter 06
Climate and Study of Glaciers
brief reversal during the LIA, when the marginal increase in glacier covering the exposed glacially polished bedrock and deposition of push moraines occurred. Climatic scenarios and circumstantial evidences suggest that the current recession would have occurred after LIA around the beginning of the 19th century. In the near future once the stratigraphic and geomorphic evidences presented in the present study are chronologically constrained, we would be in a better position to ascertain the climatic pattern that prevailed during the Kailash glaciation. In addition, chronology of past glaciation would possibly help in understanding the potential evolution of the glaciers around Mount Kailash in response to the anticipated global warming scenario. References 1. Rupper, S., Roe, G. and Gillespie, A., Spatial patterns of Holocene glacier advance and retreat in Central Asia. Quaternary
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Vernekar, A. K., Zhou, J. and Shukla, J., The effect of Eurasian snow cover on the Indian monsoon. J. Climate, 1995, 8, 248-266. 4. Owen, L. A., Debyshire, E. and Fort, M., The Quaternary glacial history of the Himalaya. Quat. Proc., 1998, 6, 91-120.
Owen, L. A., Caffee, M. W., Finkel, R. C. and Seong, Y. B., Quaternary glaciation of the Himalayan-Tibetan orogen. J. Quat. Sci., 2008,23,513-531. Benn, D. I. and Owen, L. A., The role of the Indian summer monsoon and mid-latitude westerlies in Himalayan glaciation: review and speculative discussion. J. Geol. Soc. London, 1998, 155, 353-363. Thompson, L. G., Thompson-Mosley, E., Davis, M. E., Mashiotta, T. A., Henderson, K. A., Lin, P. N. and Tandong, Y., Ice core evidence for asynchronous glaciation on the Tibetan Plateau. Quat. Int., 2006, 154-155, 3-10. Maher, B. A., Holocene variability of the East Asian summer monsoon from Chinese cave records: a re-assessment. Holocene, 2008, 18, 861-866. Owen, L. A., Gualtieri, L., Finkel, R. C., Caffee, M. W., Benn, D. I. and Sharma, M. C., Cosmogenic radionuclide dating of glacial landforms in the Lahul Himalaya, northern India: defining the timing of Late Quaternary glaciation. J.
Quat. Sci., 2001, 16, 555-563. 10. Owen, L. A., Finkel, R. C. and Caffee, M. W., A note on the extent of glaciation throughout the Himalaya during the
global Last Glacial Maximum. Quat. Sci. Rev., 2002, 21, 147-157. 11. Seong, Y. B., Owen, L. A., Yi, C. and Finkel, R. C., Quaternary glaciation of Muztang Ata and Kongur Shan: evidence
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Baltimore Symposium, IAHS Publication, May 1989, vol. 179, pp. 267-280. 15. Porter, S.C., Composite PleistocenesnowlineofOlympic MountainsandCascaderange, Washington. GSABull., 1964,75,477-482. 16. Donleet, L., Judson, S. and Kauffman, M. E., Physical Geology, Prentice-Hall, New Jersey, 1978, 5th edn, p. 482. 17. Hewitt, K., Quaternary moraines vs catastrophic rock avalanches in the Karakoram Himalaya, Northern Pakistan. Quaternary Res., 1999,51,220-237.
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