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• The climate of the Antarctic and its variability
  :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...(dark) ocean, solar radiation will be absorbed rather than reflected, and the environment will warm.
  12 KB (1,933 words) - 16:38, 22 August 2014
• The East Antarctic cryosphere in the instrumental period
  :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ..., may have forestalled an anticipated increase in snowfall associated with the global trend.
  5 KB (726 words) - 15:34, 6 August 2014
• The Greenhouse world - from the breakup of Gondwana to 34 million years ago
  :''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) - 15:34, 6 August 2014
• The Holocene
  ...s page is part of the topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...ironmental change experienced in the major regions of Antarctica which are the result of both continental and local forcing mechanisms.
  1 KB (199 words) - 15:34, 6 August 2014
• The Icehouse world - the last 34 million years
  :''This page is part of the topic [[Deep time]]'' ...G.H., Lyons, W.B., Maasch, K.A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysics'', '''4
  27 KB (4,257 words) - 15:34, 6 August 2014
• The ice sheet in the instrumental period
  ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...he spatial pattern of ice accumulation (snowfall and frost deposition) and ice ablation (melting, wind erosion and calving).
  20 KB (3,052 words) - 16:00, 6 August 2014
• The IPCC fourth assessment report
  ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...climate change resulting from increases in CO₂ concentration in the atmosphere is largely irreversible for 1,000 years after emissions stop.
  33 KB (5,155 words) - 15:34, 6 August 2014
• The physical setting of Antarctica
  :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...2''', 641-673.</ref>) and bathymetry from the General Bathymetric Chart of the Oceans (GEBCO) Centennial digital topography data (www.gebco.net).]]
  8 KB (1,295 words) - 16:38, 6 August 2014
• The transition to Holocene interglacial conditions
  :''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) - 15:34, 6 August 2014
• The Weddell Sea sector in the instrumental period
  :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...and involving ocean, atmosphere and cryosphere and a major contribution to the deep meridional overturning cell (Figure 1.9).
  15 KB (2,389 words) - 15:34, 6 August 2014
• The West Antarctic cryosphere in the instrumental period
  :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...ago and the concern driving much of the research of the West Antarctic ice sheet was whether such an eventuality was inevitable or even underway.
  17 KB (2,692 words) - 15:34, 6 August 2014