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  • ...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) - 15:45, 6 August 2014
  • ...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) - 14:33, 6 August 2014

Page text matches

  • ...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) - 15:45, 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) - 16:51, 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) - 14:33, 6 August 2014
  • ...f 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) - 12:25, 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) - 15:22, 6 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ==Antarctic stratospheric ozone in the instrumental period==
    43 KB (6,788 words) - 16:07, 22 August 2014
  • ...f 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) - 12:38, 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) - 14:33, 6 August 2014
  • ...topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...ed over [[Antarctic climate and environment change over the next 100 years|the next 100 years]].
    3 KB (503 words) - 12:42, 22 August 2014
  • :''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) - 16:17, 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) - 13:04, 22 August 2014
  • ...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) - 14:33, 6 August 2014
  • ...topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...rs. Hence studies of the past can be useful in providing insights into how the system responds and what can be expected to occur in response to future cha
    1 KB (165 words) - 14:33, 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) - 12:03, 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) - 14:33, 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) - 16:39, 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) - 16:41, 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) - 16:43, 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) - 14:33, 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) - 17:27, 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) - 15:25, 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) - 14:33, 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) - 16:49, 22 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) - 15:14, 22 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) - 14:33, 6 August 2014
  • :''This page is part of the topic [[Observations, data accuracy and tools]]'' ==The pre-satellite era==
    18 KB (2,972 words) - 16:53, 22 August 2014
  • :''This page is part of the topic [[The last million years]]'' ...Pichon, J.J. 2004. Late Qaternary sea ice history in the Indian sector of the Southern Ocean as record by diatom assemblages, ''Marine Micropaleontology'
    13 KB (2,050 words) - 14:33, 6 August 2014
  • :''This page is part of the topic [[Biological responses to climate change]]'' ...gg, I.D. 2003. Long-term isolation and recent range expansion revealed for the endemic springtail Gomphiocephalus hodgsoni from southern Victoria Land, An
    21 KB (3,069 words) - 17:14, 22 August 2014
  • :''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) - 17:17, 22 August 2014
  • :''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) - 15:38, 22 August 2014
  • :''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) - 14:34, 6 August 2014
  • ...topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...ironmental change experienced in the major regions of Antarctica which are the result of both continental and local forcing mechanisms.
    1 KB (199 words) - 14:34, 6 August 2014
  • :''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) - 14:34, 6 August 2014
  • ...topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...and the impact of this loss of ice on global sea level. Finally we review the influence of changing sea ice distributions on climate.
    1 KB (164 words) - 14:34, 6 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...="Caldeira and Duffy, 2000">Caldeira, K. and Duffy, P.B. 2000. The role of the Southern Ocean in uptake and storage of anthropogenic carbon dioxide, ''Sci
    36 KB (5,780 words) - 15:53, 6 August 2014
  • :''This page is part of the topic [[The last million years]]'' ...d Wolff, E. 2007. Orbital and millenial Antarctic climate variability over the past 800,000 years, ''Science'', '''317''', 793-796.</ref>).
    32 KB (4,956 words) - 14:34, 6 August 2014

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