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• Precipitation changes over the 21st century
  :''This page is part of the topic [[Atmospheric change over the next 100 years]]'' ...tudes is paramount for resolving the uncertainty surrounding the future of the Antarctic ice sheet.
  18 KB (2,723 words) - 15:33, 6 August 2014
• About ACCE
  ...ake place among some of the remotest and harshest environments anywhere on the Earth’s surface. ...rnational Geophysical Year of 1957-58. Many more results also emerged from the [http://www.ipy.org/ International Polar Year] of 2007-2008.
  5 KB (766 words) - 17:45, 21 August 2014
• Prospects for marine invasions by non-indigenous species
  :''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
• Recommendations
  ...ailable with which to investigate change – both in the past and over the next century, there are still major gaps in our knowledge and many areas wh ...limate change on geological time scales. In addition, scattered throughout the text there are many statements about additional research requirements.
  14 KB (2,069 words) - 16:14, 22 August 2014
• Regional climate models
  ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...n a subgrid scale – like the scale of the Antarctic Peninsula. While the spatial resolution of GCMs will increase, their capabilities will continue
  5 KB (833 words) - 15:33, 6 August 2014
• Regional patterns of holocene climate change in Antarctica
  :''This page is part of the topic [[The Holocene]]'' ...the Antarctic Peninsula region, ''The Holocene'', '''19''', 51-69.</ref>), the role of various forcing mechanisms in regional climate change is poorly des
  10 KB (1,543 words) - 15:33, 6 August 2014
• Ross Sea shelf waters in the instrumental period
  :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...Continental Shelf. In: Eds G. Spezie and G.M.R. Manzella, Oceanography of the Ross Sea Antarctica, Springer-Verlag Italia, Milano, 3-16.</ref>).
  8 KB (1,297 words) - 15:33, 6 August 2014
• Satellite observations of the Southern Ocean
  :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...-surface temperature and ice extent and visible-wavelength radiometers for ocean colour. Ensuring their continuity is of paramount importance.
  20 KB (3,084 words) - 15:57, 6 August 2014
• Sea ice change over the 21st century
  ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ..., Vinnikov, K.Y. and Cavalieri, D.J. 2006. Evaluation of the simulation of the annual cycle of Arctic and Antarctic sea ice coverages by 11 major global c
  4 KB (684 words) - 15:33, 6 August 2014
• Sea ice observations
  :''This page is part of the topic [[Observations, data accuracy and tools]]'' ==The pre-satellite era==
  18 KB (2,972 words) - 17:53, 22 August 2014
• Sea ice over the last million years
  :''This page is part of the topic [[The last million years]]'' ...2004. Late Qaternary sea ice history in the Indian sector of the Southern Ocean as record by diatom assemblages, ''Marine Micropaleontology'', '''50''', 20
  13 KB (2,050 words) - 15:33, 6 August 2014
• Sea level observations
  :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...ome locations, there were also major issues to do with datum control (e.g. the establishment of adequate local benchmark networks and maintenance of tide
  11 KB (1,784 words) - 15:33, 6 August 2014
• Small-scale processes in the Southern Ocean
  :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...uantification of such processes is a prerequisite for successful modelling the large scale conditions.
  18 KB (2,816 words) - 15:33, 6 August 2014
• Temperature changes in the instrumental period
  ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...tic can be determined using a number of different forms of data, including the ''in-situ'' observations, satellite infra-red imagery and ice core isotope
  30 KB (4,676 words) - 18:04, 22 August 2014
• Temperature changes over the 21st century
  :''This page is part of the topic [[Atmospheric change over the next 100 years]]'' [[File:Figure 5.6 - Skin temperature trend over the Twenty First Century.png|thumb|'''5.6''' Skin temperature trend over Twenty
  8 KB (1,217 words) - 15:34, 6 August 2014
• Terrestrial biological responses to climate change
  :''This page is part of the topic [[Biological responses to climate change]]'' ...al, 2006">Stevens, M.I., Greenslade, P., Hogg, I.D. and Sunnucks, P. 2006. Southern hemisphere springtails: could any have survived glaciation of Antarctica?,
  21 KB (3,069 words) - 18:14, 22 August 2014
• Terrestrial biology in the instrumental period
  ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...ninsula and in Victoria Land, terrestrial habitats exist in all sectors of the continent, and both in coastal and inland locations.
  32 KB (4,651 words) - 16:17, 6 August 2014
• Terrestrial biology over the next 100 years
  :''This page is part of the topic [[Biological responses to 21st climate climate change]]'' ...ent that have previously protected Antarctica. Antarctica contains some of the only places on Earth where natural biological phenomena can be studied in t
  22 KB (3,193 words) - 15:34, 6 August 2014
• Terrestrial biota of the Antarctic
  :''This page is part of the topic [[Biota of the Antarctic]]'' ..., and the &lsquo;sub-Antarctic&rsquo; (those islands that lie in or around the Antarctic Polar Frontal Zone (PFZ).
  22 KB (3,222 words) - 16:12, 6 August 2014
• The Amundsen and Bellingshausen seas in the instrumental period
  :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...0300-005-0058-5.</ref>). A comprehensive field study on Antarctic krill in the Amundsen Sea has yet to be conducted.
  11 KB (1,650 words) - 15:34, 6 August 2014
• The Antarctic cryosphere
  :''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).]]
  15 KB (2,479 words) - 15:34, 6 August 2014
• The Antarctic marine ecosystem in the year 2100
  :''This page is part of the topic [[Biological responses to 21st climate climate change]]'' ...scale detail in predictions of change in the physical environment, e.g. of the likelihood and extent of extreme events, and of fine scale spatial resoluti
  20 KB (3,055 words) - 15:34, 6 August 2014
• The Antarctic Peninsula cryosphere in the instrumental period
  :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ..."Vaughan, 2006">Vaughan, D.G. 2006. Recent trends in melting conditions on the Antarctic Peninsula and their implications for ice-sheet mass balance, Arct
  40 KB (6,031 words) - 18:17, 22 August 2014
• The Australian sector in the instrumental period
  :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...">Rintoul, S.R. 2007. Rapid freshening of Antarctic Bottom Water formed in the Indian and Pacific Oceans, ''Geophys. Res. Lett.'', '''34''', L06606, doi:1
  14 KB (2,205 words) - 15:34, 6 August 2014
• 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 Icehouse world - the last 34 million years
  :''This page is part of the topic [[Deep time]]'' ...ch, K.A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysics'', '''47''', RG1003, doi:1
  27 KB (4,257 words) - 15:34, 6 August 2014
• The impact of global climate change in polar marine environments
  :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...ocks (rock cod and icefish) around the Antarctic Peninsula and Scotia Arc, the populations collapsed, but legal and illegal fishing continues, especially
  14 KB (2,188 words) - 15:34, 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 open ocean system in the instrumental period
  :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...r Current. Population centres drawn by eye, relative to the Commission for the Conservation of Antarctic Living Resources (CCAMLR) Survey (from Atkinson e
  28 KB (4,437 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 role of the Antarctic in the global climate system
  :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...exchange engine and the interactions of ice shelves and land ice with the ocean and atmosphere make predictions about climate change a challenge.
  31 KB (4,808 words) - 16:51, 22 August 2014
• The Southern Ocean carbon cycle response to future climate change
  ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...Observed CO₂ emissions over the last 25 years as compared with the different IPCC emission scenarios (Raupach et al., 2007<ref name="Raupach e
  22 KB (3,567 words) - 15:34, 6 August 2014
• The Southern Ocean carbon cycle response to historical climate change
  ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...d Duffy, 2000">Caldeira, K. and Duffy, P.B. 2000. The role of the Southern Ocean in uptake and storage of anthropogenic carbon dioxide, ''Science'', '''287'
  36 KB (5,780 words) - 16:53, 6 August 2014
• The Southern Ocean in the instrumental period
  ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...nd finally the different hydrographic conditions in the northward adjacent ocean basins.
  16 KB (2,443 words) - 15:34, 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
• Understanding the seasonality of Antarctic benthic shelf communities
  :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...why most of the large predators abandon the high Antarctic at the start of the long austral winter.
  9 KB (1,434 words) - 15:34, 6 August 2014