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• Antarctic climate and environment change over the next 100 years
  ...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
• Atmospheric change over the next 100 years
  ...of the topic [[Antarctic climate and environment change over the next 100 years]]'' #[[Atmospheric circulation changes over the 21st century]]
  410 B (55 words) - 15:33, 6 August 2014
• Changes to the Terrestrial cryosphere over the next 100 years
  ...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
• 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
• Near-shore marine disturbances over the next 100 years
  :''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
• Ocean change over the next 100 years
  ...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
• 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

Page text matches

• 21st century evolution of Antarctic permafrost
  ...of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...Coast in the McMurdo Sound area (74-78&ordm;S, 165&ordm;E), and throughout the Antarctic Peninsula and its offshore islands (55-72&ordm;S, 45-70&ordm;W).
  3 KB (468 words) - 15:33, 6 August 2014
• Antarctic and Southern Ocean sea level projections
  ...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
• Antarctic climate and environment change over the next 100 years
  ...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
• 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
• Atmospheric change over the next 100 years
  ...of the topic [[Antarctic climate and environment change over the next 100 years]]'' #[[Atmospheric circulation changes over the 21st century]]
  410 B (55 words) - 15:33, 6 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 over the 21st century
  :''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
• 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 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
  ...of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...eck, 2005<ref name="Peck, 2005">Peck, L.S. 2005. Prospects for survival in the Southern Ocean: vulnerability of benthic species to temperature change, ''A
  4 KB (557 words) - 15:33, 6 August 2014
• Biological responses to climate change
  ...s page is part of the topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...arctic climate and environment change over the next 100 years|the next 100 years]].
  3 KB (503 words) - 13:42, 22 August 2014
• Changes to the Terrestrial cryosphere over the next 100 years
  ...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
• Editors
  ...ty Press. He was awarded the International Journal of Climatology Prize of the Royal Meteorological Society in 2005. ...and is often 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
• ENSO links and teleconnections to vertebrate life histories and population
  :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...increase in salps within the Southern Ocean, ''Nature'', '''432''' (7013), 100-103.</ref>).
  15 KB (2,381 words) - 15:33, 6 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 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
• 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
• 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
• Marine biota of the Antarctic
  :''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
• Marine picoplankton response to climate change
  :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...3-271.</ref>). Increases in dissolved organic matter production might fuel the growth of bacterioplankton, thereby creating a positive feedback to organic
  2 KB (305 words) - 15:33, 6 August 2014
• Meteorological and ozone observing in the Antarctic
  :''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
• Near-shore marine disturbances over the next 100 years
  :''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
• Observations of Antarctic permafrost
  :''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
• Observations of marine biology
  :''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
• Observations of the ice sheet
  :''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
• Ocean change over the next 100 years
  ...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
• Pathways of research in cold-adapted organisms and climate change
  :''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
• 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&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
• 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
  ...ble 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 where w ...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
• 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
• Sea ice change over the 21st century
  ...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
• 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 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
• 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 marine ecosystem in the year 2100
  :''This page is part of the topic [[Biological responses to 21st climate climate change]]'' ...theless, physical predictions have improved considerably compared to a few years ago, because they now include some measurements of regional as well as glob
  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 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 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]]'' ...on, G.H., Lyons, W.B., Maasch, K.A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysi
  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