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  • ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...Observed CO<sub>2</sub> emissions over the last 25 years as compared with the different IPCC emission scenarios (Raupach et al., 2007<ref name="Raupach e
    22 KB (3,567 words) - 14:34, 6 August 2014
  • ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...000. The role of the Southern Ocean in uptake and storage of anthropogenic carbon dioxide, ''Science'', '''287''', 620-622.</ref>).
    36 KB (5,780 words) - 15:53, 6 August 2014

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  • ...itions across the Southern Ocean, ocean conditions, the sea ice extent and the terrestrial and marine biology. ...emainder of the Nineteenth Century and it was not possible to venture into the inhospitable interior of Antarctica.
    3 KB (501 words) - 15:48, 6 August 2014
  • ...f the changes observed in recent decades. This is particularly the case in the ocean where we have few long time series of physical measurements and remar ...as near-surface air temperature it is possible to use the projections from the various models to derive various estimates of how temperature may change ov
    5 KB (788 words) - 15:49, 6 August 2014
  • ...ciation, retreat of the ice sheet and its effects on global sea level, and the changing distribution of sea ice and its effect on climate are then describ ...tanding of the climate and biological changes that might be anticipated in the near future (Chapter 5).
    17 KB (2,554 words) - 15:45, 6 August 2014
  • ...rld where greenhouse gas concentrations are much higher than occurred over the last few centuries. ...SCAR Advisory Group on ACCE] has overall responsibility for the content of the wiki and plan to keep it up to date as new research results emerge. We hope
    4 KB (504 words) - 16:51, 21 August 2014
  • ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ==Antarctic stratospheric ozone in the instrumental period==
    43 KB (6,788 words) - 16:07, 22 August 2014
  • ...s page is part of the topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...equence of events with better resolution both temporally (for instance, in the phasing of changes in Antarctic climate, environmental parameters and atmos
    7 KB (1,082 words) - 14:33, 6 August 2014
  • ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...reproduce reality. Such reality checks are often crude, given that most of the commonly used GCMs do not operate at a finer scale than one-degree squares.
    13 KB (2,051 words) - 14:33, 6 August 2014
  • :''This page is part of the topic [[The last million years]]'' ...xt.png|thumb|'''3.9''' Main climatic events of the last 1 Million years in the Antarctic context]]
    35 KB (5,415 words) - 14:33, 6 August 2014
  • :''This page is part of the topic [[Regional patterns of holocene climate change in Antarctica]]'' ==Deglaciation history and the Pleistocene-Holocene transition==
    38 KB (5,787 words) - 16:39, 22 August 2014
  • :''This page is part of the topic [[The Holocene]]'' ...variability must be taken into account in understanding modern climate and the potential for future climate change.
    39 KB (5,945 words) - 14:33, 6 August 2014
  • :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...ated with the climate regime can be interpreted as major driving forces on the large scale biogeography of marine water breathing animals. These relations
    25 KB (3,817 words) - 14:33, 6 August 2014
  • :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...2002">Wiencke, C. and Clayton, M.N. 2002. Antarctic Seaweeds, (Synopses of the Antarctic Benthos. Ed.: J. W. W&auml;gele and J. Sieg ; Vol. 9), Ruggell :
    11 KB (1,587 words) - 14:33, 6 August 2014
  • ...e gas concentrations increase at the present rate then temperatures across the continent will increase by several degrees and there will be about one thir ==The Geological Dimension (Deep Time)==
    48 KB (7,673 words) - 17:27, 22 August 2014
  • ...r, J., and The ACCE Consortium. 2009. Review: Antarctic climate change and the environment, Antarctic Science, 1-23.</ref>). ...nline PDF version of the report is available to download without cost from the SCAR web site (http://www.scar.org/publications/occasionals/acce.html) or h
    142 KB (22,142 words) - 15:25, 6 August 2014
  • :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...c contaminants and greenhouse gases may reduce the value of Antarctica and the surrounding Southern Ocean for research on evolutionary and ecophysiologica
    38 KB (5,770 words) - 14:33, 6 August 2014
  • :''This page is part of the topic [[Biota of the Antarctic]]'' ...rs of the Antarctic shelf comparable to classic evolutionary sites such as the Galapagos.
    43 KB (6,450 words) - 14:33, 6 August 2014
  • :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...rrigno, J. 2005, Retreating glacier fronts on the Antarctic Peninsula over the past half-century, ''Science'', '''308''', 541-544.</ref>).
    54 KB (8,443 words) - 16:49, 22 August 2014
  • ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ==Simulation of present-day conditions in the Southern Ocean.==
    33 KB (5,321 words) - 14:57, 22 August 2014
  • ...ailable with which to investigate change &ndash; both in the past and over the next century, there are still major gaps in our knowledge and many areas wh ...limate change on geological time scales. In addition, scattered throughout the text there are many statements about additional research requirements.
    14 KB (2,069 words) - 15:14, 22 August 2014
  • ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...terotrophic flagellates and other small protists, which play a key role in the cycling of material (e.g. excretion of nitrogen) and in controlling microal
    18 KB (2,786 words) - 14:33, 6 August 2014
  • ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...ninsula and in Victoria Land, terrestrial habitats exist in all sectors of the continent, and both in coastal and inland locations.
    32 KB (4,651 words) - 15:17, 6 August 2014
  • :''This page is part of the topic [[Deep time]]'' ...ical Research'', '''99''', 15115-15139.</ref>). The shaded area represents the modelled error envelope.]]
    20 KB (3,076 words) - 14:34, 6 August 2014
  • ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...climate change resulting from increases in CO<sub>2</sub> concentration in the atmosphere is largely irreversible for 1,000 years after emissions stop.
    33 KB (5,155 words) - 14:34, 6 August 2014
  • :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...r Current. Population centres drawn by eye, relative to the Commission for the Conservation of Antarctic Living Resources (CCAMLR) Survey (from Atkinson e
    28 KB (4,437 words) - 14:34, 6 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...heat exchange engine and the interactions of ice shelves and land ice with the ocean and atmosphere make predictions about climate change a challenge.
    31 KB (4,808 words) - 15:51, 22 August 2014
  • ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...Observed CO<sub>2</sub> emissions over the last 25 years as compared with the different IPCC emission scenarios (Raupach et al., 2007<ref name="Raupach e
    22 KB (3,567 words) - 14:34, 6 August 2014
  • ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...000. The role of the Southern Ocean in uptake and storage of anthropogenic carbon dioxide, ''Science'', '''287''', 620-622.</ref>).
    36 KB (5,780 words) - 15:53, 6 August 2014
  • ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...orcing (storm tracks) and finally the different hydrographic conditions in the northward adjacent ocean basins.
    16 KB (2,443 words) - 14:34, 6 August 2014
  • :''This page is part of the topic [[The last million years]]'' ...d Wolff, E. 2007. Orbital and millenial Antarctic climate variability over the past 800,000 years, ''Science'', '''317''', 793-796.</ref>).
    32 KB (4,956 words) - 14:34, 6 August 2014

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