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  • File:Figure 1.10 - Major currents south of 20S.png
    ...hue, 2007">McCartney, M.S. and Donohue, K.A. 2007. A deep cyclonic gyre in the Australian-Antarctic Basin, ''Progress in Oceanography'', '''75''', 675-750
    (601 × 589 (308 KB)) - 15:31, 6 August 2014
  • File:Figure 4.28 - Vertical distribution of turbulent diapycnal diffusivity along the rim of the Scotia Sea.png
    ...and Visbeck, M. 2004. Widespread intense turbulent mixing in the Southern Ocean, ''Science'', '''303''', 210-213.</ref>).
    (536 × 543 (332 KB)) - 15:31, 6 August 2014
  • File:Figure 3.18 - February SSTs and sea ice duration in core SO136-111 and insolation curves.png
    ...2004. Late Qaternary sea ice history in the Indian sector of the Southern Ocean as record by diatom assemblages, ''Marine Micropaleontology'', '''50''', 20
    (553 × 559 (212 KB)) - 15:31, 6 August 2014
  • File:Figure 2.18 - Southern Ocean scatterometer and thermal infrared data acquired on 15 Jan 1995.png
    ...tterometer winds, Weather and Forecasting, 14, 867 877.</ref>; courtesy of the American Meteorological Society).
    (553 × 546 (376 KB)) - 15:31, 6 August 2014
  • File:Figure 4.58 - Sea-air CO2 flux anomalies in the Southern Ocean.png
    ...., Metzl, N., Gillett, N. and Heimann, M. 2007. Saturation of the Southern Ocean CO2 Sink Due to Recent Climate Change, ''Science'', '''316''', 1735-1738, d
    (338 × 354 (63 KB)) - 15:31, 6 August 2014
  • File:Figure 5.25 - Predicted aragonite saturation state of the surface ocean in the year 2100.png
    ...line represents the saturation horizon and shows that much of the Southern Ocean (&lt;50&ordm;S) is expected to be under-saturated with respect to aragonite
    (645 × 276 (136 KB)) - 15:31, 6 August 2014
  • File:Figure 3.14 - Climate and environmental records of Termination I.png
    ...d Wolff, E. 2007. Orbital and millenial Antarctic climate variability over the past 800,000 years, ''Science'', '''317''', 793-796.</ref>).
    (418 × 649 (125 KB)) - 15:31, 6 August 2014
  • File:Figure 3.17 - Sea ice distribution at the Southern Ocean EPILOG-LGM time slice.png
    ...Sea-surface temperature and sea ice distribution of the Southern Ocean at the EPILOG Last Glacial Maximum-a circum-Antarctic view based on siliceous micr
    (552 × 520 (145 KB)) - 15:31, 6 August 2014
  • File:Figure 2.12 - Example figure produced using the Southern Ocean Atlas.png
    Example figure produced using the Southern Ocean Atlas (http://woceatlas.tamu.edu/). Dots show all data from 1900 to 2007 in
    (491 × 163 (110 KB)) - 15:31, 6 August 2014
  • File:Figure 2.13b - JCOMMOPS Southern Ocean region sub-surface profiles as of February 2008.png
    Sub-surface profiles available in the Southern Ocean region from JCOMMOPS (as of February 2008).
    (265 × 256 (95 KB)) - 15:31, 6 August 2014
  • File:Figure 2.29 - Residual of regression of bivalve species richness against sampling effort, from SOMBASE.png
    ...ues below the mean; grey areas: no representative data. This example shows the high spatial heterogeneity obviously shaped by ecological conditions and be
    (324 × 278 (97 KB)) - 15:31, 6 August 2014
  • File:Figure 4.50 - Acute temperature influences on Antarctic invertebrates.png
    ...name="Peck, 2005">Peck, L.S. 2005. Prospects for survival in the Southern Ocean: vulnerability of benthic species to temperature change, ''Antarctic Sci.''
    (544 × 230 (28 KB)) - 15:31, 6 August 2014
  • File:Figure 4.55 - The annual cycle atmosphere-ocean CO2 transport in the Southern Ocean.png
    ...and Schauer, B. 2006. Summer and Winter Air-Sea CO2 Fluxes in the Southern Ocean, Deep-Sea Research II, 53.</ref>).
    (570 × 281 (36 KB)) - 15:31, 6 August 2014
  • Antarctic and Southern Ocean sea level projections
    ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...n-uniform due to the influence of ocean currents and spatial variations in ocean warming. Global warming from increasing greenhouse gas concentrations is a
    16 KB (2,491 words) - 13:16, 22 August 2014
  • Antarctic climate and environment change in the instrumental period
    ...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
  • Antarctic climate and environment change over the next 100 years
    ...e changes observed in recent decades. This is particularly the case in the ocean where we have few long time series of physical measurements and remarkably ...ls to derive various estimates of how temperature may change over land and ocean.
    5 KB (788 words) - 16:49, 6 August 2014
  • Antarctic climate and environment history in the pre-instrumental period
    ...ciation, retreat of the ice sheet and its effects on global sea level, and the changing distribution of sea ice and its effect on climate are then describ ...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
  • Antarctic Climate Change and the Environment
    ...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
  • Antarctic deglaciation and its impact on global sea level
    :''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
  • Antarctic sea ice cover in the instrumental period
    ...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
  • Atmospheric chemistry changes over the 21st century
    :''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
  • Atmospheric chemistry in the instrumental period
    ...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
  • Atmospheric circulation changes in the instrumental period
    ...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
  • Atmospheric circulation changes over the 21st century
    :''This page is part of the topic [[Atmospheric change over the next 100 years]]'' ...istribution of sea ice, and the seasonal to interannual variability of the Southern Hemisphere.
    29 KB (4,462 words) - 17:11, 22 August 2014
  • Attribution of ice sheet changes in the instrumental period
    :''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
  • Biological modelling and bioregionalization
    ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...nd Harris, 2005">Beaman, R.J. and Harris, P.T. 2005. Bioregionalization of the George V Shelf, East Antarctica, ''Cont. Shelf Res.'', '''25''', 1657-1691.
    8 KB (1,225 words) - 15:33, 6 August 2014
  • Biological response of birds and mammals
    :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...ssing on individual physiology and behaviour is important, because that is the level at which natural selection works, and other responses ultimately depe
    16 KB (2,488 words) - 15:33, 6 August 2014
  • Biological responses to 21st climate climate change
    ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...name="Peck, 2005">Peck, L.S. 2005. Prospects for survival in the Southern Ocean: vulnerability of benthic species to temperature change, ''Antarctic Sci.''
    4 KB (557 words) - 15:33, 6 August 2014
  • Biota of the Antarctic
    :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...and bound to be upset by rapid changes such as those that are occurring at the present time.
    9 KB (1,315 words) - 15:33, 6 August 2014
  • Changes in Antarctic snowfall over the past 50 years
    ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...en Broeke, M.R., Reijmer, C.H. and Van Meijgaard, E. 2006. Reassessment of the Antarctic surface mass balance using calibrated output of a regional atmosp
    20 KB (3,125 words) - 15:33, 6 August 2014
  • Changes in sea ice extent through the Holocene
    :''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
  • Changes to the Terrestrial cryosphere over the next 100 years
    ...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
  • Concluding remarks on the pre-instrumental period
    ...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
  • Coupled atmosphere-ocean models
    ...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
  • Deglaciation of the continental shelf, coastal margin and continental interior
    :''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
  • ENSO links and teleconnections to vertebrate life histories and population
    :''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
  • Future developments in Antarctic observation
    :''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
  • Glacial interglacial cycles
    :''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
  • Holocene climate change in East Antarctica (EA)
    :''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
  • Holocene climate change in the Antarctic Peninsula (AP)
    :''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
  • Holocene climate change in the Ross Sea region (RS)
    :''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
  • Holocene climate changes
    :''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
  • Impacts of instrumental period climate change on invertebrates
    :''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
  • In-situ ocean observations
    :''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
  • Key points - 2009 version
    ...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
  • Key points - 2013 version
    ...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
  • Long term sea level change in the instrumental period
    ...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
  • Marine and terrestrial pollution
    :''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
  • Marine biological responses to climate change
    :''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
  • Marine biology over the next 100 years
    :''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

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