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• Coupled atmosphere-ocean models
  ...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) - 15:33, 6 August 2014
• Deglaciation of the continental shelf, coastal margin and continental interior
  :''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
• ENSO links and teleconnections to vertebrate life histories and population
  :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...ong-term decline in krill stocks and increase in salps within the Southern Ocean, ''Nature'', '''432''' (7013), 100-103.</ref>).
  15 KB (2,381 words) - 15:33, 6 August 2014
• Future developments in Antarctic observation
  :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...ed increasingly in recent decades and this trend is certain to continue in the future.
  7 KB (1,040 words) - 16:16, 22 August 2014
• Glacial interglacial cycles
  :''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
• Holocene climate change in East Antarctica (EA)
  :''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
• Holocene climate change in the Antarctic Peninsula (AP)
  :''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
• Holocene climate change in the Ross Sea region (RS)
  :''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
• Holocene climate changes
  :''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
• Impacts of instrumental period climate change on invertebrates
  :''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) - 15:33, 6 August 2014
• In-situ ocean observations
  :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...d Asper, 2007">Smith, W. and Asper, V.A. 2007. New Ways to Collect Data in the Antarctic, EOS, Transactions American Geophysical Union, 88, no. 48, 525.</
  17 KB (2,672 words) - 15:50, 6 August 2014
• Key points - 2009 version
  ...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
• Key points - 2013 version
  ...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) - 16:25, 6 August 2014
• Long term sea level change in the instrumental period
  ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...is small compared to what it was following the LGM Transition and through the Holocene.
  8 KB (1,342 words) - 15:33, 6 August 2014
• Marine and terrestrial pollution
  :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...ouse gases may reduce the value of Antarctica and the surrounding Southern Ocean for research on evolutionary and ecophysiological processes and as an ideal
  38 KB (5,770 words) - 15:33, 6 August 2014
• Marine biological responses to climate change
  :''This page is part of the topic [[Biological responses to climate change]]'' ...nctions is unknown. Bivalves appear to have been particularly badly hit in the intervening 35 Ma and it is possible that this happened for a variety of re
  54 KB (8,173 words) - 15:33, 6 August 2014
• Marine biology over the next 100 years
  :''This page is part of the topic [[Biological responses to 21st climate climate change]]'' ...species is much lower (and marine alien species very much lower) south of the Front, although there is evidence that some species exchange occurs in both
  9 KB (1,386 words) - 15:33, 6 August 2014
• Marine biota of the Antarctic
  :''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) - 15:33, 6 August 2014
• Marine picoplankton response to climate change
  :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...tionally to inform future models and enhance our understanding of Southern Ocean microbial ecology.
  2 KB (305 words) - 15:33, 6 August 2014
• Meteorological and ozone observing in the Antarctic
  :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...atic stations. A further boost to the observing network has taken place in the International Polar Year of 2007 &ndash; 2008.
  59 KB (9,046 words) - 15:33, 6 August 2014