Arid
DOI10.5194/acp-13-7007-2013
Atmospheric mercury over sea ice during the OASIS-2009 campaign
Steffen, A.1,2; Bottenheim, J.1; Cole, A.1; Douglas, T. A.3; Ebinghaus, R.2,4; Friess, U.5; Netcheva, S.1; Nghiem, S.6; Sihler, H.5; Staebler, R.1
通讯作者Steffen, A.
来源期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
ISSN1680-7316
EISSN1680-7324
出版年2013
卷号13期号:14页码:7007-7021
英文摘要

Measurements of gaseous elemental mercury (GEM), reactive gaseous mercury (RGM) and particulate mercury (PHg) were collected on the Beaufort Sea ice near Barrow, Alaska, in March 2009 as part of the Ocean-Atmosphere-Sea Ice-Snowpack (OASIS) and OASIS-Canada International Polar Year programmes. These results represent the first atmospheric mercury speciation measurements collected on the sea ice. Concentrations of PHg averaged 393.5 pg m(-3) (range 47.1-900.1 pg m(-3)) and RGM concentrations averaged 30.1 pg m(-3) (range 3.5-105.4 pg m(-3)) during the two-week-long study. The mean concentration of GEM during the study was 0.59 ng m(-3) (range 0.01-1.51 ng m(-3)) and was depleted compared to annual Arctic ambient boundary layer concentrations. It is shown that when ozone (O-3) and bromine oxide (BrO) chemistry were active there is a positive linear relationship between GEM and O-3, a negative one between PHg and O-3, a positive correlation between RGM and BrO, and none between RGM and O-3. For the first time, GEM was measured simultaneously over the tundra and the sea ice. The results show a significant difference in the magnitude of the emission of GEM from the two locations, with significantly higher emission over the tundra. Elevated chloride levels in snow over sea ice are proposed to be the cause of lower GEM emissions over the sea ice because chloride has been shown to suppress photoreduction processes of RGM to GEM in snow. Since the snowpack on sea ice retains more mercury than inland snow, current models of the Arctic mercury cycle may greatly underestimate atmospheric deposition fluxes because they are based predominantly on land-based measurements. Land-based measurements of atmospheric mercury deposition may also underestimate the impacts of sea ice changes on the mercury cycle in the Arctic. The predicted changes in sea ice conditions and a more saline future snowpack in the Arctic could enhance retention of atmospherically deposited mercury and increase the amount of mercury entering the Arctic Ocean and coastal ecosystems.


类型Article
语种英语
国家Canada ; Germany ; USA
收录类别SCI-E
WOS记录号WOS:000322448300018
WOS关键词SOURCE-RECEPTOR RELATIONSHIPS ; SPRINGTIME DEPLETION ; GASEOUS MERCURY ; NY-ALESUND ; DERIVE INFORMATION ; ELEMENTAL MERCURY ; CRYSTAL-FORMATION ; ARCTIC SNOWPACK ; HG-P ; OZONE
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/175988
作者单位1.Environm Canada, Air Qual Proc Res Sect, Toronto, ON M3H 5T4, Canada;
2.Univ Luneburg, ISEC, D-21335 Luneburg, Germany;
3.US Army Cold Reg Res & Engn Lab, Ft Wainwright, AK 99703 USA;
4.Helmholtz Zentrum Geesthacht, Inst Coastal Res, Dept Environm Chem, D-21502 Geesthacht, Germany;
5.Heidelberg Univ, Inst Environm Phys, D-69120 Heidelberg, Germany;
6.CALTECH, Jet Prop Lab, Pasadena, CA USA
推荐引用方式
GB/T 7714
Steffen, A.,Bottenheim, J.,Cole, A.,et al. Atmospheric mercury over sea ice during the OASIS-2009 campaign[J],2013,13(14):7007-7021.
APA Steffen, A..,Bottenheim, J..,Cole, A..,Douglas, T. A..,Ebinghaus, R..,...&Staebler, R..(2013).Atmospheric mercury over sea ice during the OASIS-2009 campaign.ATMOSPHERIC CHEMISTRY AND PHYSICS,13(14),7007-7021.
MLA Steffen, A.,et al."Atmospheric mercury over sea ice during the OASIS-2009 campaign".ATMOSPHERIC CHEMISTRY AND PHYSICS 13.14(2013):7007-7021.
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