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A twentieth century major soluble ion record of dust and anthropogenic pollutants from Inilchek Glacier, Tien Shan
Grigholm, B.1,2; Mayewski, P. A.1,2; Aizen, V.3; Kreutz, K.1,2; Aizen, E.3; Kang, S.4,5; Maasch, K. A.1,2; Sneed, S. B.1,2
刊名JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
2017-02-16
卷号122期号:3页码:1884-1900
ISSN号2169-897X
DOI10.1002/2016JD025407
通讯作者Grigholm, B.(bjorn.grigholm@maine.edu)
英文摘要Using a high-resolution (similar to 18 samples/year) major soluble ion record (Na+, K+, Mg2+, Ca2+, Cl-, NO3-, and SO42-) covering the period 1908-1995 A. D. from the Inilchek Glacier, Tien Shan, Kyrgyzstan, we provide a detailed climate and environmental proxy record for the region. Chemical concentrations, empirical orthogonal function analyses, and noncrustal excess calculations are used to identify natural and potential anthropogenic depositional trends. Dominant dust proxy species (i. e., Ca2+) reveal highest concentrations during the 1950s-1970s, with declining decadal trends through the end of the record. These trends likely reflect decreases in central Asian dust storm activity post-1950, which has been associated with coupled atmospheric circulation variability and anthropogenic activities. Comparison between Ca2+ and ERA-Interim (1979-1995) climate reanalysis data indicates a strong relationship to spring (March-May) geopotential height patterns in northwest China and southern Siberia associated with the Siberian High. Noncrustal contribution (excess) estimates of NO3-, K+, SO42-, and Cl- concentrations suggest discernable anthropogenic inputs began between the 1950s and 1970s, increased into the middle/late 1980s, and declined in the 1990s. Excess trends coincide with Former Soviet Union consumption, production, and emission of fossil fuels and fertilizers, reflecting the rapid growth of agriculture and industry, as well as economic declines in the middle to late 1980s/early 1990s. Excess-Cl- trends reflect timings that coincide with the construction of the Pavlodar Chemical Plant and the military production of Cl-2 in Kazakhstan. NOAA Hybrid Single-Particle Lagrangian Integrated Trajectory back trajectory frequency analysis suggests eastern Uzbekistan (e. g., Fergana Valley), Kyrgyzstan, and southern Kazakhstan as the primary pollutant sources to the study region.
收录类别SCI
WOS关键词ALPINE ICE-CORE ; CENTRAL-ASIA ; TIBETAN PLATEAU ; SULFATE ; EMISSIONS ; STORMS ; CHEMISTRY ; CHINA ; ALPS ; AIR
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000396119200030
内容类型期刊论文
URI标识http://www.corc.org.cn/handle/1471x/2557584
专题寒区旱区环境与工程研究所
通讯作者Grigholm, B.
作者单位1.Univ Maine, Climate Change Inst, Orono, ME 04469 USA
2.Univ Maine, Sch Earth & Climate Sci, Orono, ME 04469 USA
3.Univ Idaho, Dept Geog, Moscow, ID 83843 USA
4.Chinese Acad Sci, State Key Lab Cryospher Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou, Peoples R China
5.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Grigholm, B.,Mayewski, P. A.,Aizen, V.,et al. A twentieth century major soluble ion record of dust and anthropogenic pollutants from Inilchek Glacier, Tien Shan[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2017,122(3):1884-1900.
APA Grigholm, B..,Mayewski, P. A..,Aizen, V..,Kreutz, K..,Aizen, E..,...&Sneed, S. B..(2017).A twentieth century major soluble ion record of dust and anthropogenic pollutants from Inilchek Glacier, Tien Shan.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,122(3),1884-1900.
MLA Grigholm, B.,et al."A twentieth century major soluble ion record of dust and anthropogenic pollutants from Inilchek Glacier, Tien Shan".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 122.3(2017):1884-1900.
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