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  • ...age 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) - 17:39, 22 August 2014
  • ...age is part of the topic [[Regional patterns of holocene climate change in Antarctica]]'' ==Deglaciation history the Pleistocene-Holocene transition==
    17 KB (2,705 words) - 17:43, 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) - 15:33, 6 August 2014
  • ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...m-mechanical model for the flow of anisotropic polar ice to the EDML core, Antarctica.
    33 KB (5,053 words) - 15:33, 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) - 18:27, 22 August 2014
  • :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...s, D.K.A. and Smith, R.C. 2007. Climate change and the marine ecosystem of the western Antarctic Peninsula, ''Phil. Trans. R. Soc. B'', '''362''', 149-166
    25 KB (3,663 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...ecoming more homogeneous as these few winners spread from port to port and the many losers will be native species with restricted distributions (endemics)
    13 KB (2,063 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Deep time]]'' ...ate of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysics'', '''47''', RG1003, doi:10.1029/2007RG000231.</ref>).]]
    27 KB (4,257 words) - 15:34, 6 August 2014
  • ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...to the current climate, where flow exactly compensates the spatial pattern of ice accumulation (snowfall and frost deposition) and ice ablation (melting,
    20 KB (3,052 words) - 16:00, 6 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' [[File:Figure 1.1a - Map of Antarctica.png|thumb|'''1.1a''' A map of Antarctica showing selected topographic features and locations.]]
    8 KB (1,295 words) - 16:38, 6 August 2014

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