Chemical composition and isotopic signatures of ice and snow over a Himalayan Glacier (Satopanth) in India

• Published in: SN Applied Sciences
• Main Authors: Panicker, A. S., Sandeep, K., Gautam, A. S., Gandhi, Naveen, Beig, G., Nainwal, H. C., Rao, P. S. P., Safai, P. D., Das, S., Waghmare, V.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Nature Switzerland AG 2019
• Subjects: QE Geology; ice core
• Online Access: http://repository.ias.ac.in/133369/; http://repository.ias.ac.in/133369/1/s42452-019-0966-6.pdf; https://doi.org/10.1007/s42452-019-0966-6

This study reports the chemical composition and isotopic signatures of snow and ice over a Himalayan Glacier in India. An observational campaign was carried out from September 22, 2016, to October 2, 2016, over Satopanth in central Himalaya. The pH value of ice and snow, respectively, was 5.6 ± 0.4 and 5.9 ± 0.35 over the glacier, indicating moderate acidity of the glacier components. Calcium (Ca2+) was the dominant component in snow (35.2%), while sulfate (SO42−) was dominant in ice samples (52.7%). The neutralization factor was estimated to find the extent of neutralization of acidic fractions by basic components. It is found that Ca2+ was the prominent neutralizing factor both in snow and ice over the region. Oxygen and hydrogen isotopic analyses of snow, surface layer ice and debris-covered ice suggest that the moisture source is common for all three components. δD and d-excess values of snow at Satopanth are different than that of those for Chorabari, Dokriani and Tiprabank Glacier, indicating the plausibility of different sources of moisture for these glaciers. Limited observations suggest that the interaction of ice with the debris has no impact on the isotopic signatures of the ice over the region; such non-alteration of isotopic signatures makes the region important for ice core-based paleoclimatic studies.