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• Antarctic and Southern Ocean sea level projections
  ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...and and Antarctica). The amount of thermal expansion is non-uniform due to the influence of ocean currents and spatial variations in ocean warming. Global
  16 KB (2,491 words) - 13:16, 22 August 2014
• Antarctic climate and environment change over the next 100 years
  ...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) - 16:49, 6 August 2014
• Antarctic climate and environment history in the pre-instrumental period
  ...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
• Antarctic sea ice cover in the instrumental period
  ...is page is part of 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
• Atmospheric change over the next 100 years
  ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' #[[Atmospheric circulation changes over the 21st century]]
  410 B (55 words) - 15:33, 6 August 2014
• Atmospheric chemistry changes over the 21st century
  :''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
• Atmospheric chemistry in the instrumental period
  ...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) - 17:07, 22 August 2014
• Atmospheric circulation changes in the instrumental period
  ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...random sample, and can ‘describe’ a significant proportion of the total circulation variability.
  54 KB (8,177 words) - 13:38, 22 August 2014
• Atmospheric circulation changes over the 21st century
  :''This page is part of the topic [[Atmospheric change over the next 100 years]]'' ...he distribution of sea ice, and the seasonal to interannual variability of the Southern Hemisphere.
  29 KB (4,462 words) - 17:11, 22 August 2014
• Attribution of ice sheet changes in the instrumental period
  :''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
• Changes in Antarctic snowfall over the past 50 years
  ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ==General spatial and temporal characteristics of Antarctic snowfall==
  20 KB (3,125 words) - 15:33, 6 August 2014
• Changes in sea ice extent through the Holocene
  :''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
• Changes to the Terrestrial cryosphere over the next 100 years
  ...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
• Conclusions on the ice sheet in the instrumental period
  :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...he ice sheet places different parts in markedly different positions within the global climate system and subjects them to different environmental drivers.
  3 KB (475 words) - 15:33, 6 August 2014
• Coupled atmosphere-ocean models
  ...rt 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
• Glacial interglacial cycles
  :''This page is part of the topic [[The last million years]]'' ...ng|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 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]]'' ...per, 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.</ref>).
  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