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  • :''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
  • ...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
  • ...s page is part of the topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...equence of events with better resolution both temporally (for instance, in the phasing of changes in Antarctic climate, environmental parameters and atmos
    7 KB (1,082 words) - 15:33, 6 August 2014
  • ...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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''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
  • ...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
  • ...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
  • ...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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''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
  • :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...shortcomings, so their results have to be considered with as much care as the ones derived from observations alone. Indeed, some models throw up contradi
    8 KB (1,343 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...e and increasingly, biological studies. In this section we examine some of the major classes of models used in Antarctic studies.
    2 KB (322 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...rrigno, J. 2005, Retreating glacier fronts on the Antarctic Peninsula over the past half-century, ''Science'', '''308''', 541-544.</ref>).
    54 KB (8,443 words) - 17:49, 22 August 2014
  • ...tained from satellite systems that have become increasingly important over the last couple of decades. ...ng to be employed in biology &ndash; a trend that seems set to continue in the future.
    2 KB (307 words) - 16:44, 6 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...arctic environment, such as meteorology, solar-terrestrial interactions in the Earth&rsquo;s outer atmosphere (known as &lsquo;geospace&rsquo;), coastal s
    5 KB (752 words) - 15:09, 22 August 2014
  • :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...ues below the mean; grey areas: no representative data. This example shows the high spatial heterogeneity obviously shaped by ecological conditions and be
    23 KB (3,516 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...tion about the processes that operate to change the Antarctic environment. The combination of fieldwork, aircraft, and satellite measurements has revealed
    52 KB (8,045 words) - 15:43, 22 August 2014
  • ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ==Simulation of present-day conditions in the Southern Ocean.==
    33 KB (5,321 words) - 15:57, 22 August 2014
  • ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...ost and physical realism. This is especially true for ocean models because the computational cost is always high, and can be hundreds of times that of a c
    37 KB (5,859 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...s, D.K.A. and Smith, R.C. 2007. Climate change and the marine ecosystem of the western Antarctic Peninsula, ''Phil. Trans. R. Soc. B'', '''362''', 149-166
    25 KB (3,663 words) - 15:33, 6 August 2014
  • :''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&rsquo;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 &ndash; 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 &ndash; 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

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