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  • :''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
  • ...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
  • :''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
  • ...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
  • ...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
  • :''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
  • :''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
  • :''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
  • ...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
  • :''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
  • :''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
  • :''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
  • :''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
  • ...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
  • :''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
  • :''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
  • ...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
  • :''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
  • :''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
  • :''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

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