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From Ice to Space

The Antarctic Atmosphere

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Exploring the Last Continent

Abstract

The atmosphere over Antarctica is pristine, dry and isolated. This is because it is very far from all sources of manmade emissions, is extremely cold and completely surrounded by the enormous Southern Ocean. It is, however, home to unusual chemical and physical processes that have a global significance. In this chapter, we start by considering some fundamental concepts used to describe the Earth’s atmosphere. We then focus on measurements of past and present carbon dioxide concentrations from Antarctica, the stratospheric ozone hole, and atmospheric chemistry occurring near ground level. Finally, we consider some connections between these apparently distinct phenomena in order to illustrate the critical role the Antarctic atmosphere plays in connecting global land, ice and oceans, as well as different geographical areas of the Earth.

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Bibliography

  • British Antarctic Survey, The Ozone Hole (2012). http://www.antarctica.ac.uk/about_bas/publications/bas_the_ozone_hole.pdf

  • Carlisle R (2004) Scientific American inventions and discoveries. Wiley, New York, p 351. ISBN 0-471-24410-4

    Google Scholar 

  • EPICA Community Members (2004) Eight glacial cycles from an Antarctic ice core. Nature 429:623–628

    Article  Google Scholar 

  • Etheridge DM, Steele LP, Langenfelds RL, Francey RJ, Barnola J-M, Morgan VI (1996) Natural and anthropogenic changes in atmospheric CO2 over the last 1000 years from air in Antarctic ice and firn. J Geophys Res 101:4115–4128

    Article  CAS  Google Scholar 

  • Farman JC, Gardiner BG, Shanklin JD (1985) Large losses of total ozone in Antarctica reveal seasonal ClOx/NOx interaction. Nature 35:207–210

    Article  Google Scholar 

  • Grannas AM, Jones AE, Dibb J, Ammann M, Anastasio C, Beine HJ, Bergin M, Bottenheim J, Boxe CS, Carver G, Chen G, Crawford JH, DominĂ© F, Frey MM, GuzmĂ¡n MI, Heard DE, Helmig D, Hoffmann MR, Honrath RE, Huey LG, Hutterli M, Jacobi HW, KlĂ¡n P, Lefer B, McConnell J, Plane J, Sander R, Savarino J, Shepson PB, Simpson WR, Sodeau JR, von Glasow R, Weller R, Wolff EW, Zhu T (2007) An overview of snow photochemistry: evidence, mechanisms and impacts. Atmos Chem Phys 7:4329–4373. doi:10.5194/acp-7-4329-2007, http://www.wmo.int/pages/prog/arep/gaw/ozone_2010/ozone_asst_report.html

  • IPCC (2013) Summary for policymakers. In: Stocker TF, Qin D, Plattner G-K, Tignor M, Allen SK, Boschung J, Nauels A, Xia Y, Bex V, Midgley PM (eds) Climate change 2013: the physical science basis. Contribution of working group I to the fifth assessment report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge (in press)

    Google Scholar 

  • Jones AE (2008) The Antarctic ozone hole. Phys Educ 43(4):358–366, www.iop.org/journals/physed

  • Jouzel J et al (2007) Orbital and millennial Antarctic climate variability over the last 800,000 years. Science 317:793–796

    Article  CAS  Google Scholar 

  • LĂ¼thi D, le Floch M, Bereiter B, Blunier T, Barnola J-M, Siegenthaler U, Raynaud D, Jouzel J, Fischer H, Kawamura K, Stocker T (2008) High-resolution carbon dioxide concentration record 650,000–800,000 years before present. Nature 453:379–382

    Article  Google Scholar 

  • MacFarling Meure C (2004) The natural and anthropogenic variations of carbon dioxide, methane and nitrous oxide during the Holocene from ice core analysis. PhD thesis, University of Melbourne

    Google Scholar 

  • MacFarling Meure C, Etheridge D, Trudinger C, Steele P, Langenfelds R, van Ommen T, Smith A, Elkins J (2006) The law dome CO2, CH4 and N2O ice core records extended to 2000 years BP. Geophys Res Lett 33(14):L14810. doi:10.1029/2006GL026152

    Article  Google Scholar 

  • Molina MJ, Rowland FS (1974) Stratospheric sink for chlorofluorocarbons: chlorine atom-catalysed destruction of ozone. Nature 249:810–814

    Article  CAS  Google Scholar 

  • Pfaffhuber KA, Berg T, Hirdman D, Stohl A (2012) Atmospheric mercury observations from Antarctica: seasonal variation and source and sink region calculations. Atmos Chem Phys 12:3241–3251

    Article  CAS  Google Scholar 

  • Salmon RA, Carlson DJ (2007) International polar year – the poles and the planet. In: Stewart C, Green A (eds) EcoScience: the 34th Harry Messel International Science School. Science Foundation of Physics within the University of Sydney, Sydney, pp 146–161

    Google Scholar 

  • Simpson WR, von Glasow R, Riedel K, Anderson P, Ariya P, Bottenheim J, Burrows J, Carpenter LJ, FrieĂŸ U, Goodsite ME, Heard D, Hutterli M, Jacobi H-W, Kaleschke L, Neff B, Plane J, Platt U, Richter A, Roscoe H, Sander R, Shepson P, Sodeau J, Steffen A, Wagner T, Wolff E (2007) Halogens and their role in polar boundary-layer ozone depletion. Atmos Chem Phys 7:4375–4418. doi:10.5194/acp-7-4375-2007

    Article  CAS  Google Scholar 

  • Steffen A, Douglas T, Amyot M, Ariya P, Aspmo K, Berg T, Bottenheim J, Brooks S, Cobbett F, Dastoor A, Dommergue A, Ebinghaus R, Ferrari C, Gardfeldt K, Goodsite ME, Lean D, Poulain AJ, Scherz C, Skov H, Sommar J, Temme C (2008) A synthesis of atmospheric mercury depletion event chemistry in the atmosphere and snow. Atmos Chem Phys 8:1445–1482. doi:10.5194/acp-8-1445-2008

    Article  CAS  Google Scholar 

  • Turner JT, Lachlan-Cope TA, Colwell S, Marshall GJ, Connolley WM (2006) Significant warming of the Antarctic winter troposphere. Science 311:1914–1917

    Article  CAS  Google Scholar 

  • Turner, J, Bindschadler, R, Convey P, di Prisco G, Fahrbach E, Gutt J, Hodgson D, Mayewski P, Summerhayes C (2009) Antarctic climate change and the environment. SCAR, Cambridge, http://www.scar.org/publications/occasionals/acce.html

  • Turner JT, Comiso JC, Marshall GJ, Lachlan-Cope TA, Bracegirdle T, Maksym T, Meredith MP, ZZhaomin W, Orr A (2009) Non-annular atmospheric circulation change induced by stratospheric ozone depletion and its role in the recent increase of Antarctic sea ice extent. Geophys Res Lett 36:L08502. doi:10.1029/2009GL037524

    Google Scholar 

  • Von Glasow R (2008) Recent developments in tropospheric halogen chemistry. Science features, IGACtivities. http://www.uea.ac.uk/~fkd06bju/papers/vonGlasow_IGAC_2008.pdf

  • World Meteorological Organization, Scientific Assessment of Ozone Depletion (2010) Global ozone research and monitoring project, report 52, Geneva, Switzerland, p 516

    Google Scholar 

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Correspondence to Rhian A. Salmon .

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Salmon, R.A., Jones, A.E. (2015). From Ice to Space. In: Liggett, D., Storey, B., Cook, Y., Meduna, V. (eds) Exploring the Last Continent. Springer, Cham. https://doi.org/10.1007/978-3-319-18947-5_8

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