| Miller, M.M., J.S. Leventhal, and W.F. Libby, Tritium in Mt. Everest ice-annual glacier accumulation and climatology at great equatorial altitudes, J. Geophys. Res., 70, 3885-3888, 1965. |
.... corresponds to summer precipitation (Figure 4a) Therefore given the regional distribution of summer autumn air temperatures, significant variations in composition of d 18 O (Figure 4a) reflect summer autumn snow brought by different air masses: monsoon circulation and westerly disturbances [Miller et al. 1965; Barry, 1981; Inoue, 1976] The stratigraphic analyses of snow firn core from the Xixibangma glacier (Figure 5b) revealed two periods. Subannual analysis of each accumulation snow firn layer in the core from the Xixibangma glacier indicates also two air masses with different isotopic composition ....
Miller, M.M., J.S. Leventhal, and W.F. Libby, Tritium in Mt. Everest ice-annual glacier accumulation and climatology at great equatorial altitudes, J. Geophys. Res., 70, 3885-3888, 1965.
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