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  • ...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) - 16:45, 6 August 2014
  • ...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) - 15:33, 6 August 2014

Page text matches

  • ...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) - 16:45, 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) - 17:51, 21 August 2014
  • :''This page is part of the topic [[The last million years]]'' ...e-dynamic reconstructions of the Greenland and Antarctic ice sheets during the glacial cycles, ''Quaternary Science Reviews'', '''21''', 203-231.</ref>).
    21 KB (3,294 words) - 15:33, 6 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...were reliant on sparse ship observations that were mainly collected during the summer months.
    22 KB (3,536 words) - 13:25, 22 August 2014
  • :''This page is part of the topic [[Atmospheric change over the next 100 years]]'' ==Antarctic stratospheric ozone over the next 100 years==
    27 KB (4,305 words) - 16:22, 6 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ==Antarctic stratospheric ozone in the instrumental period==
    43 KB (6,788 words) - 17:07, 22 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...random sample, and can &lsquo;describe&rsquo; a significant proportion of the total circulation variability.
    54 KB (8,177 words) - 13:38, 22 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...ange. The inescapable fact is that ice sheet behaviour manifests itself as the superposition of multiple responses on multiple time scales to multiple env
    13 KB (1,943 words) - 15:33, 6 August 2014
  • ...topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...ed over [[Antarctic climate and environment change over the next 100 years|the next 100 years]].
    3 KB (503 words) - 13:42, 22 August 2014
  • :''This page is part of the topic [[The Holocene]]'' ...ial to use proxy records to represent how Antarctic sea ice has changed in the past.
    24 KB (3,785 words) - 17:17, 22 August 2014
  • ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...uperposition of the continuing gradual response to past climate change and the more rapid responses to present and future changes.
    26 KB (4,124 words) - 14:04, 22 August 2014
  • ...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) - 15:33, 6 August 2014
  • ...topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...rs. Hence studies of the past can be useful in providing insights into how the system responds and what can be expected to occur in response to future cha
    1 KB (165 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[The last million years]]'' ...contributor to post-LGM sea level rise, it has been the most sensitive of the Antarctic ice sheets to climate change and sea level rise (Domack et al., 2
    22 KB (3,430 words) - 13:03, 22 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) - 15:33, 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) - 17:39, 22 August 2014
  • :''This page is part of the topic [[Regional patterns of holocene climate change in Antarctica]]'' ==Deglaciation history and the Pleistocene-Holocene transition==
    32 KB (5,127 words) - 17:41, 22 August 2014
  • :''This page 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
  • ...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

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