Recent high-resolution glaciochemical record from a Dasuopu firn core of middle Himalayas |
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Authors: | Wang PengLing Yao TanDong Tian LiDe Wu GuangJian Li Zhen Yang Wei |
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Institution: | (1) Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China;(2) National Key Laboratory of Cryospheric Sciences, Chinese Academy of Sciences, Lanzhou, 730000, China;(3) Graduate University of the Chinese Academy of Sciences, Beijing, 100049, China |
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Abstract: | A 16.8 m firn core of middle Himalayas was recovered on the col of Dasuopu glacier in August 2006, being 7000 m above sea
level. A total of 317 samples were measured for stable oxygen isotope ratios (δ
18O) and major ion concentrations (Na+, NH
4
+
, K+, Mg2+, Ca2+, Cl−, SO
4
2−
, and NO
3
−
). The firn core dating and seasonal partitioning were carried out based on the marked seasonal variations along the stable
oxygen isotopes and crustal species (Ca2+, Mg2+) profiles. The multi-parameters and high-resolution glaciochemical data set of Dasuopu firn core recorded the detailed chemical
characteristics of precipitation in high-elevation region, middle Himalayas, since 1991 A.D., which mainly originated from
the crustal and anthropogenic sources, while the sea-salt contribution was minor. The seasonal variability of major ion concentrations
was dominated by the seasonal alternation of the prevalent air mass, atmospheric circulation situation and precipitation regime.
Linear regression analysis indicated that most of the variance in annual ionic fluxes can be explained by a linear dependence
on snow accumulation rate.
Supported by the National Basic Research Program of China (Grant No. 2005CB422004), and the National Natural Science Foundation
of China (Grant Nos. 40571039 and 40121101) |
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Keywords: | glaciochemical record seasonal variation South Asian monsoon middle Himalaya |
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