中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Resolving the impact of stratosphere-to-troposphere transport on the sulfur cycle and surface ozone over the Tibetan Plateau using a cosmogenic S-35 tracer

文献类型:期刊论文

作者Kang, SC; Kang, SC (Kang, Shichang)3,4,5; Chan, CY (Chan, Chuen-Yu)1; Thiemens, MH (Thiemens, Mark H.)6; Thiemens, MH; Chan, CY; Lin, M (Lin, Mang)6; Zhang, ZS (Zhang, Zhisheng)7; Su, L (Su, Lin)8; Hill-Falkenthal, J (Hill-Falkenthal, Jason)6
刊名JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
出版日期2016
卷号121期号:1页码:439-456
关键词Dispersion Model Flexpart Summer Monsoon Season Elemental Composition Atmospheric Sulfate Downward Transport Mineral Dust Black-carbon Air-quality South-asia Nam Co
DOI10.1002/2015JD023801
文献子类Article
英文摘要The Himalayas were recently identified as a global hot spot for deep stratosphere-to-troposphere transport (STT) in spring. Although the STT in this region may play a vital role in tropospheric chemistry, the hydrological cycle and aquatic ecosystems in Asia, there is no direct measurement of a chemical stratospheric tracer to verify and evaluate its possible impacts. Here we use cosmogenic S-35 as a tracer for air masses originating in the stratosphere and transported downward. We measure concentrations of S-35 in fresh surface snow and river runoff samples collected from Mount Everest in April 2013 to be more than 10 times higher than previously reported by any surface measurement, in support of the Himalayas as a gateway of springtime STT. In light of this result, measurements of (SO2)-S-35 and (SO42-)-S-35 at Nam Co in spring 2011 are reanalyzed to investigate the magnitudes of stratospheric air masses from the Himalayas to the tropospheric sulfur cycle and surface O-3 level over the Tibetan Plateau. A simple one-box model reveals that the oxidative lifetime of SO2 is reduced in aged STT plumes. Triple oxygen isotopic measurements of sulfate samples suggest that enhanced O-3 levels may shift the oxidation pathway of SO2 in the troposphere, which may be constrained by further intensive sampling and measurements. Comparison with surface O-3 measurements and traditional meteorological tracing methods shows that S-35 is a potentially unique and sensitive tracer to quantify the contribution of stratospheric air to surface O-3 levels in fresh or aged STT plumes.
学科主题自然地理学
语种英语
WOS记录号WOS:000369845300027
源URL[http://ir.itpcas.ac.cn/handle/131C11/7779]  
专题青藏高原研究所_图书馆
通讯作者Kang, SC; Thiemens, MH; Chan, CY
作者单位1.Chinese Acad Sci, Inst Earth Environm, Xian, Peoples R China
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China
3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
4.Chinese Acad Sci, State Key Lab Cryospher Sci Cold & Arid Reg Envir, Lanzhou, Peoples R China
5.Chinese Acad Sci, Engn Res Inst, Lanzhou, Peoples R China
6.Univ Calif San Diego, Dept Chem & Biochem, La Jolla, CA 92093 USA
7.South China Inst Environm Sci, Minist Environm Protect, Guangzhou, Guangdong, Peoples R China
8.Hong Kong Univ Sci & Technol, Sch Sci, Environm Sci Programs, Hong Kong, Hong Kong, Peoples R China
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Kang, SC,Kang, SC ,Chan, CY ,et al. Resolving the impact of stratosphere-to-troposphere transport on the sulfur cycle and surface ozone over the Tibetan Plateau using a cosmogenic S-35 tracer[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2016,121(1):439-456.
APA Kang, SC.,Kang, SC .,Chan, CY .,Thiemens, MH .,Thiemens, MH.,...&Zhang, GS .(2016).Resolving the impact of stratosphere-to-troposphere transport on the sulfur cycle and surface ozone over the Tibetan Plateau using a cosmogenic S-35 tracer.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,121(1),439-456.
MLA Kang, SC,et al."Resolving the impact of stratosphere-to-troposphere transport on the sulfur cycle and surface ozone over the Tibetan Plateau using a cosmogenic S-35 tracer".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 121.1(2016):439-456.

入库方式: OAI收割

来源:青藏高原研究所

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