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  • :''This page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...1970s microwave instruments on polar orbiting satellites have enabled sea ice observations to be made year-round and even during periods of complete clou
    22 KB (3,536 words) - 13:25, 22 August 2014

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  • :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...lly by melting of land-based sources of ice (glaciers and ice caps and the ice sheets of Greenland and Antarctica). The amount of thermal expansion is non
    16 KB (2,491 words) - 13:16, 22 August 2014
  • ...orological conditions across the Southern Ocean, ocean conditions, the sea ice extent and the terrestrial and marine biology. ...this really began the period of organised scientific investigation in the Antarctic. Most of these stations were not operated for long periods, which is a hand
    3 KB (501 words) - 16:48, 6 August 2014
  • ...t for both scientists and policymakers concerned with issues as diverse as sea-level rise and fish stocks. A major problem is that we still have a poor un ...ojections for temperature and precipitation were used to estimate how much sea level would rise under various greenhouse gas emission scenarios. In the fo
    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. ...nt interglacial, the Holocene is described in detail from a combination of ice cores, marine sediments, lake sediments and terrestrial records with a focu
    17 KB (2,554 words) - 16:45, 6 August 2014
  • ...as changed from Deep Time until the present day. It also considers how the Antarctic environment may change over the next century in a world where greenhouse ga ...fic Committee on Antarctic Research ([http://www.scar.org/ SCAR]) known as Antarctic Climate Change and the Environment (ACCE), which is described in [[About AC
    4 KB (504 words) - 17:51, 21 August 2014
  • ...at the LGM from ice-dynamic reconstructions of the Greenland and Antarctic ice sheets during the glacial cycles, ''Quaternary Science Reviews'', '''21''', ...ce the eustatic contribution and so there is a continuous fall in relative sea level like that seen in areas such as Hudson Bay or Sweden today.
    21 KB (3,294 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...1970s microwave instruments on polar orbiting satellites have enabled sea ice observations to be made year-round and even during periods of complete clou
    22 KB (3,536 words) - 13:25, 22 August 2014
  • ==Antarctic stratospheric ozone over the next 100 years== ...averaged over some period, and it is the most accurate diagnostic of total Antarctic ozone loss.</li>
    27 KB (4,305 words) - 16:22, 6 August 2014
  • :''This 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 [[Antarctic climate and environment change in the instrumental period]]'' ...08. Here the SAM is in its positive phase with negative anomalies over the Antarctic and positive anomalies over the Southern Ocean.]]
    54 KB (8,177 words) - 13:38, 22 August 2014
  • ...ulation in the warming of the Antarctic Peninsula, the distribution of sea ice, and the seasonal to interannual variability of the Southern Hemisphere. ...y, analyses of sea level pressure have revealed secular decreases over the Antarctic, associated with increases in mid-latitude westerlies, a poleward displacem
    29 KB (4,462 words) - 17:11, 22 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...such as recent/anthropogenic climate change. The inescapable fact is that ice sheet behaviour manifests itself as the superposition of multiple responses
    13 KB (1,943 words) - 15:33, 6 August 2014
  • ...rt of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...y production, and are either supported or reduced by the occurrence of sea ice (Beaman and Harris, 2005<ref name="Beaman and Harris, 2005">Beaman, R.J. an
    8 KB (1,225 words) - 15:33, 6 August 2014
  • ...sonality of high latitudes, phenology is a key aspect of the adaptation of Antarctic organisms and populations to change, and can be used to evaluate the match ...., Baroni, C., Lambert, D.M. 2005. Microevolution and mega-icebergs in the Antarctic, ''Proc. Natl. Acad. Sci.'', '''102''', 16717-16722</ref>). This suggests t
    16 KB (2,488 words) - 15:33, 6 August 2014
  • :''This 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
  • ...e it will be essential to use proxy records to represent how Antarctic sea ice has changed in the past. ...ichon, J.J. and Burckle, L.H. 1998b. Reappraisal of Antarctic seasonal sea-ice at the Last Glacial Maximum, ''Geophysical Research Letters'', '''25''', 27
    24 KB (3,785 words) - 17:17, 22 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...xy data and analogues exist. The broad range of time scale response of the ice sheet guarantees that future behaviour will be composed of a superposition
    26 KB (4,124 words) - 14:04, 22 August 2014
  • :''This 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]]'' ...e been considered unlikely even a decade ago. The geographic extent of the ice sheet places different parts in markedly different positions within the glo
    3 KB (475 words) - 15:33, 6 August 2014
  • ...rt of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...r strengths and weaknesses, before presenting some results relevant to the Antarctic from the models used in the IPCC AR4.
    13 KB (2,051 words) - 15:33, 6 August 2014

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