Search results

Jump to: navigation, search

Page title matches

  • ...operated for long periods, which is a handicap when trying to investigate climate change over the last century. The ocean areas around the Antarctic have been investigated far less than the continent itself. Here we are reli
    3 KB (501 words) - 16:48, 6 August 2014
  • Determining how the environment of the Antarctic will evolve over the next century presents many challenges, yet it is a que ...</ref>) gave a wide range of projections for some aspects of the Antarctic climate system. In the case of sea ice extent that was not entirely surprising, sin
    5 KB (788 words) - 16:49, 6 August 2014
  • ...obal sea level, and the changing distribution of sea ice and its effect on climate are then described. ...ges of the Holocene that are being used to inform our understanding of the climate and biological changes that might be anticipated in the near future (Chapte
    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 ...tee on Antarctic Research ([http://www.scar.org/ SCAR]) known as Antarctic Climate Change and the Environment (ACCE), which is described in [[About ACCE]]. Th
    4 KB (504 words) - 17:51, 21 August 2014
  • :''This page is part of the topic [[Regional patterns of holocene climate change in Antarctica]]'' ...nsula.png|thumb|'''3.26''' Selected Holocene environmental changes &ndash; Antarctic Peninsula]]
    32 KB (5,127 words) - 17:41, 22 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' In the summer, when the sun is above the horizon for long periods, the Antarctic receives more solar radiation than the tropics, but the highly reflective i
    12 KB (1,933 words) - 16:38, 22 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...shelves and land ice with the ocean and atmosphere make predictions about climate change a challenge.
    31 KB (4,808 words) - 16:51, 22 August 2014

Page text matches

  • :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...t 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
  • :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...ified additional contribution from a dynamic response of the Greenland and Antarctic ice sheets to global warming. The inset shows the 2001 projection compared
    16 KB (2,491 words) - 13:16, 22 August 2014
  • ...operated for long periods, which is a handicap when trying to investigate climate change over the last century. The ocean areas around the Antarctic have been investigated far less than the continent itself. Here we are reli
    3 KB (501 words) - 16:48, 6 August 2014
  • Determining how the environment of the Antarctic will evolve over the next century presents many challenges, yet it is a que ...</ref>) gave a wide range of projections for some aspects of the Antarctic climate system. In the case of sea ice extent that was not entirely surprising, sin
    5 KB (788 words) - 16:49, 6 August 2014
  • ...obal sea level, and the changing distribution of sea ice and its effect on climate are then described. ...ges of the Holocene that are being used to inform our understanding of the climate and biological changes that might be anticipated in the near future (Chapte
    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 ...tee on Antarctic Research ([http://www.scar.org/ SCAR]) known as Antarctic Climate Change and the Environment (ACCE), which is described in [[About ACCE]]. Th
    4 KB (504 words) - 17:51, 21 August 2014
  • ...l changes at the LGM from ice-dynamic reconstructions of the Greenland and Antarctic ice sheets during the glacial cycles, ''Quaternary Science Reviews'', '''21 ...lative sea level curves for the South Shetland Islands and Marguerite Bay, Antarctic Peninsula, ''Quaternary Science Reviews'', '''24''', 1203-1216.</ref>).
    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]]'' This section considers the variability and trend in Antarctic sea ice area and extent over the last century. This time splits into two ve
    22 KB (3,536 words) - 13:25, 22 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' [[Category:The Antarctic atmosphere]]
    410 B (55 words) - 15:33, 6 August 2014
  • ==Antarctic stratospheric ozone over the next 100 years== ...y cannot be used for predictions of the future. Instead, coupled Chemistry-Climate Models are used. Those whose results are described below vary in their skil
    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
  • ...spects of importance include the role of circulation in the warming of the Antarctic Peninsula, the distribution of sea ice, and the seasonal to interannual var ...se changes in circulation have been demonstrated in station-based data and climate model realizations of the Twentieth and Twenty First Centuries.
    29 KB (4,462 words) - 17:11, 22 August 2014
  • ...sheet to a particular causal event or events such as recent/anthropogenic climate change. The inescapable fact is that ice sheet behaviour manifests itself a ...l, W., Rivera, A. and Thomas, R. 2004a. Accelerated ice discharge from the Antarctic Peninsula following the collapse of Larsen B ice shelf, Geophys. Res. Let.,
    13 KB (1,943 words) - 15:33, 6 August 2014
  • ...rt of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...dquo; structuring communities of the sublittoral Antarctic macrobenthos, ''Antarctic Sci.'', '''12''' (3), 297-313.</ref>) to others with possibly the lowest co
    8 KB (1,225 words) - 15:33, 6 August 2014
  • ..., Hoegh-Guldberg, O. and Bairlein, F. 2002. Ecological responses to recent climate change, ''Nature'', '''416''', 389-395.</ref>). Focussing on individual phy ...R&eacute;ale, D., McAdam, A.G. and Boutin, S. 2004. Keeping pace with fast climate change: can Arctic life count on evolution? Integrative Comp Biol., 44, 140
    16 KB (2,488 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...gests that long-term survival of these organisms under conditions of rapid climate change may be compromised.
    4 KB (557 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...climate and biological changes that might be anticipated over [[Antarctic climate and environment change over the next 100 years|the next 100 years]].
    3 KB (503 words) - 13:42, 22 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...squo;s extreme environments without also addressing the impacts of current climate changes on organisms whose adaptations to climatic conditions have slowly e
    9 KB (1,315 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' Permafrost temperatures and active layer depth are sensitive indicators of climate because they integrate different climatic factors (i.e. air temperature, se
    6 KB (847 words) - 16:11, 6 August 2014

View (previous 20 | next 20) (20 | 50 | 100 | 250 | 500)