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- W2078591997 abstract "Abstract A 40.9 m ice core was recovered from Far East Rongbuk Glacier (FER), Qomolangma (Mount Everest), Himalaya, and an 80.4 m core from neighboring East Rongbuk Glacier (ER). Both are dated by seasonal variations of δ 18 O and major-ionic profiles, together with references of β-activity peaks. In this paper we compare the chemical records of these two cores to show post-depositional modification processes. The smoothed β 18 O profiles of the two cores show a similar trend. However, the mean β 18 O value of the FER core for the period 1954—96 is 3.12%o less than that of the corresponding part of the ER core, and the major-ionic profiles of the two cores differ considerably. We suggest that melting-away of the snow layer deposited during the pre-monsoon season may account for lower β 18 O values of the FER than of the ER core, and higher terrestrial ion concentrations in the FER core for the period 1957-63 may contribute to changes by chemical reactions in the presence of snowmelting. The significantly decreased NH 4 and, to a lesser degree, SO 4 2 concentrations in the FER core could be caused by the ion elution process that moved most chemicals away with runoff." @default.
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- W2078591997 date "2002-01-01" @default.
- W2078591997 modified "2023-10-13" @default.
- W2078591997 title "Comparison of two ice-core chemical records recovered from the Qomolangma (Mount Everest) region, Himalaya" @default.
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- W2078591997 doi "https://doi.org/10.3189/s0260305500268110" @default.
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