Oxygen and deuterium isotope characteristics of Teesta river catchment from Sikkim Himalaya, India: Implications of different moisture sources
Author:
Affiliation:
1. Birbal Sahni Institute of Palaeosciences
2. Physical Research Laboratory (PRL)
Publisher
Geochemical Society of Japan
Subject
Geochemistry and Petrology,Geophysics
Link
https://www.jstage.jst.go.jp/article/geochemj/54/5/54_2.0604/_pdf
Reference70 articles.
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2. Ali, S. N., Dubey, J., Morthekai, P., Sharma, A., Singh, R. and Prizomwala, S. (2019) Climate forcing and the initiation of glacier advance during MIS-2 in the North Sikkim Himalaya, India. J. Asian Earth Sci. 174, 381−388.
3. Annamalai, H., Hamilton, K. and Sperber, K. R. (2007) The South Asian summer monsoon and its relationship with ENSO in the IPCC AR4 simulations. J. Clim. 20(6), 1071−1092.
4. Benn, D. I. and Owen, L. A. (1998) The role of the Indian summer monsoon and the midlatitude westerlies in Himalayan glaciation: review and speculative discussion. J. Geol. Soc. 155, 353−363.
5. Chang, C. P., Ding, Y. H. and Lau, G. N.C. (eds.) (2011) The Global Monsoon System: Research and Forecast. 2nd ed., World Scientific Publishing, Singapore.
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