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Sökning: WFRF:(Granfors Anna 1978) > (2016) > Antarctic winter me...

Antarctic winter mercury and ozone depletion events over sea ice

Nerentorp, Michelle, 1986 (författare)
Chalmers tekniska högskola,Chalmers University of Technology
Gårdfeldt, Katarina, 1959 (författare)
Chalmers tekniska högskola,Chalmers University of Technology
Jourdain, B. (författare)
Université Grenoble Alpes,Grenoble Alpes University
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Abrahamsson, Katarina, 1957 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences,University of Gothenburg
Granfors, Anna, 1978 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences,University of Gothenburg
Ahnoff, Martin (författare)
Gothenburg University,Göteborgs universitet,Institutionen för marina vetenskaper,Department of marine sciences,University of Gothenburg
Dommergue, A. (författare)
Université Grenoble Alpes,Grenoble Alpes University
Mejean, G. (författare)
Université Grenoble Alpes,Grenoble Alpes University
Jacobi, H. W. (författare)
Université Grenoble Alpes,Grenoble Alpes University
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 (creator_code:org_t)
Elsevier BV, 2016
2016
Engelska.
Ingår i: Atmospheric Environment. - : Elsevier BV. - 1352-2310 .- 1873-2844. ; 129, s. 125-132
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • During atmospheric mercury and ozone depletion events in the springtime in polar regions gaseous elemental mercury and ozone undergo rapid declines. Mercury is quicldy transformed into oxidation products, which are subsequently removed by deposition. Here we show that such events also occur during Antarctic winter over sea ice areas, leading to additional deposition of mercury. Over four months in the Weddell Sea we measured gaseous elemental, oxidized, and particulate-bound mercury, as well as ozone in the troposphere and total and elemental mercury concentrations in snow, demonstrating a series of depletion and deposition events between July and September. The winter depletions in July were characterized by stronger correlations between mercury and ozone and larger formation of particulate-bound mercury in air compared to later spring events. It appears that light at large solar zenith angles is sufficient to initiate the photolytic formation of halogen radicals. We also propose a dark mechanism that could explain observed events in air masses coming from dark regions. Br-2 that could be the main actor in dark conditions was possibly formed in high concentrations in the marine boundary layer in the dark. These high concentrations may also have caused the formation of high concentrations of CHBr3 and CH2I2 in the top layers of the Antarctic sea ice observed during winter. These new findings show that the extent of depletion events is larger than previously believed and that winter depletions result in additional deposition of mercury that could be transferred to marine and terrestrial ecosystems.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Kemi (hsv//swe)
NATURAL SCIENCES  -- Chemical Sciences (hsv//eng)

Nyckelord

Mercury
Ozone
Depletion event
Antarctica
Sea ice
dissolved gaseous mercury
atmospheric mercury
polar sunrise
surface
ozone
springtime depletion
molecular halogens
coastal antarctica
elemental mercury
tropospheric bro
arctic-ocean
Environmental Sciences & Ecology
Meteorology & Atmospheric Sciences
elemental mercury

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