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  • ...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
  • ...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
  • ...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
  • :''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 [[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
  • ...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 [[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

  • ...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
  • ...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
  • ...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
  • ...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
  • ...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
  • ...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
  • :''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
  • :''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
  • :''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
  • ...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
  • ...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
  • ...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
  • ...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
  • :''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
  • :''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

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