Abstract
A total of 14 surface snow (0–10 cm) samples were collected along the climbing route (6500–8844 m a.s.l.) on the northern slope of Mt. Qomolangma in May, 2005. Analysis of elemental concentrations in these samples showed that there are no clear trends for element variations with elevation due to redistribution of surface snow by strong winds during spring. In addition, local crustal aerosol inputs also have an influence on elemental composition of surface snow. Comparison between elemental concentration datasets of 2005 and 1997 indicated that data from 2005 were of higher quality. Elemental concentrations (especially for heavy metals) at Mt. Qomolangma are comparable with polar sites, and far lower than large cities. This indicates that anthropogenic activities and heavy metal pollution have little effect on the Mt. Qomolangma atmospheric environment, which can be representative of the background atmospheric environment.
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Supported by the National Natural Science Foundation of China (Grant Nos. 40401054, 90411003 and 40121101), the National Basic Research Program of China (Grant No.2005CB422004), Social Commonweal Research Project of Ministry of Science and Technology of China (Grant No.2005DIA3J106),the “Talent Project” and Innovation Project (Grant No.KZCX3-SW-334/339) of CAS, and Dean Foundation of CAS
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Zhang, Q., Kang, S., Cong, Z. et al. Elemental composition in surface snow from the ultra-high elevation area of Mt. Qomolangma (Everest). Chin. Sci. Bull. 53, 289–294 (2008). https://doi.org/10.1007/s11434-007-0446-z
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DOI: https://doi.org/10.1007/s11434-007-0446-z