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  • File:Figure 3.1 - Map of Antarctica showing locations of selected deep ice and sediment cores.png
    ...at Seymour Island (SI), James Ross Island (JRI), Alexander Island (AI) and the Beardmore Glacier region (BG).
    (512 × 422 (151 KB)) - 15:30, 6 August 2014
  • File:Figure 4.25 - Amundsen Sea bathymetric chart and hydrographic stations of different cruises.png
    ...ers refer to the Nathaniel B. Palmer (NBP), the James Clark Ross (JCR) and the Polarstern (ANT).
    (637 × 481 (343 KB)) - 15:30, 6 August 2014
  • File:Figure 3.10 - Accurately dated Antarctic ice-core records and the comparison with sea level proxies.png
    ...ans, J. 2005. Modelled atmospheric temperatures and global sea levels over the past million years, ''Nature'', '''437''', 125-128.</ref>) and regression a
    (611 × 396 (118 KB)) - 15:30, 6 August 2014
  • File:Figure 1.5 - Antarctic ice thickness.png
    ...nent ice shelves that represent floating extensions of the continental ice sheet. From Lythe, Vaughan and BEDMAP Consortium, 2001.
    (624 × 542 (347 KB)) - 15:31, 6 August 2014
  • File:Figure 3.8 - Lithological column for the upper 600m of the AND-1B drillcore.png
    ...lch, T. and Williams, T. 2009. Obliquity-paced Pliocene West Antarctic ice sheet oscillations, ''Nature'', '''458''', 322-328.</ref>).
    (562 × 694 (486 KB)) - 15:31, 6 August 2014
  • File:Figure 4.41 - Pictorial view of the ocean-ice system of the Ross Sea.png
    ...ere (wavy vertical line) while the remainder circulated under the floating ice shelf causing basal melting. (illustration courtesy of National Geographic)
    (533 × 342 (194 KB)) - 15:31, 6 August 2014
  • File:Figure 2.33 - Bed elevations of the Amundsen Sea Embayment.png
    ...n shows that the recent surveys provided a more detailed representation of the subglacial topography.
    (447 × 250 (342 KB)) - 15:31, 6 August 2014
  • File:Figure 3.19a - Antarctic and Greenland holocene climate change compared using ice core data.png
    ...Annals of Glaciology'', '''39''', 127-132.</ref>, 2005). Green bar denotes the 8,800-8,200 year ago event seen in many globally distributed records associ
    (414 × 807 (400 KB)) - 15:31, 6 August 2014
  • File:Figure 4.8c - Winter season temperature trends reconstructed using infrared satellite data.png
    ...and Shindell, D.T. 2009. Warming of the Antarctic ice-sheet surface since the 1957 International Geophysical Year, ''Nature'', '''457''', 459-462.</ref>)
    (455 × 500 (175 KB)) - 15:31, 6 August 2014
  • File:Figure 3.7 - View of the Victoria Land coast off Cape Roberts during Oligocene and early Miocene times.png
    ...e filled circle. TAM = Transantarctic Mountains, EAIS = East Antarctic Ice Sheet.
    (479 × 471 (169 KB)) - 15:31, 6 August 2014
  • ...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
  • ...itions across the Southern Ocean, ocean conditions, the sea ice extent and the terrestrial and marine biology. ...emainder of the Nineteenth Century and it was not possible to venture into the inhospitable interior of Antarctica.
    3 KB (501 words) - 16:48, 6 August 2014
  • ...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
  • ...and its effects on global sea level, and the changing distribution of sea ice and its effect on climate are then described. ...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
  • ...rld where greenhouse gas concentrations are much higher than occurred over the last few centuries. ...SCAR Advisory Group on ACCE] has overall responsibility for the content of the wiki and plan to keep it up to date as new research results emerge. We hope
    4 KB (504 words) - 17:51, 21 August 2014
  • :''This page is part of the topic [[The last million years]]'' ...e-dynamic reconstructions of the Greenland and Antarctic ice sheets during the glacial cycles, ''Quaternary Science Reviews'', '''21''', 203-231.</ref>).
    21 KB (3,294 words) - 15:33, 6 August 2014
  • ...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
  • :''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
  • ...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
  • ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...random sample, and can &lsquo;describe&rsquo; a significant proportion of the total circulation variability.
    54 KB (8,177 words) - 13:38, 22 August 2014
  • :''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
  • :''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
  • ...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
  • ...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]]'' ...ter resolution both temporally (for instance, in the phasing of changes in Antarctic climate, environmental parameters and atmospheric composition) and spatiall
    7 KB (1,082 words) - 15:33, 6 August 2014
  • :''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
  • ...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
  • :''This page is part of the topic [[The last million years]]'' ...nsula Climate Variability: Historical and Paleoenvironmental Perspectives, Antarctic Research Series, 79. American Geophysical Union.</ref>).
    22 KB (3,430 words) - 13:03, 22 August 2014
  • ...ty Press. He was awarded the International Journal of Climatology Prize of the Royal Meteorological Society in 2005. ...n quoted commenting on glaciological impacts of the climate on the world's ice sheets and glaciers.
    7 KB (1,089 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]]'' ...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
  • :''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
  • ...rt of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...n of a continuum-mechanical model for the flow of anisotropic polar ice to the EDML core, Antarctica.
    33 KB (5,053 words) - 15:33, 6 August 2014
  • ...ill increase by several degrees and there will be about one third less sea ice.</li> ==The Geological Dimension (Deep Time)==
    48 KB (7,673 words) - 18:27, 22 August 2014
  • ...CE 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
  • :''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 [[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 [[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]]'' ...es. 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 [[Observations, data accuracy and tools]]'' ...., Shiklomanov, N.I. and Hinkel, K.M. 1998. Spatial temporal attributes of the active-layer thickness record, Barrow, Alaska, USA. In: Lewkowicz, AG., All
    23 KB (3,347 words) - 19:33, 22 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
  • :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...d Smith, R.C. 2007. Climate change and the marine ecosystem of the western Antarctic Peninsula, ''Phil. Trans. R. Soc. B'', '''362''', 149-166.</ref>).
    25 KB (3,663 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Atmospheric change over the next 100 years]]'' ...for resolving the uncertainty surrounding the future of the Antarctic ice sheet.
    18 KB (2,723 words) - 15:33, 6 August 2014

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