Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.5194/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
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ISSN | 1680-7316 |
EISSN | 1680-7324 |
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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