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File:Figure 3.19a - Antarctic and Greenland holocene climate change compared using ice core data.png ...Kreutz, K. 2004b. A 700 year record of Southern Hemisphere extra-tropical climate variability, ''Annals of Glaciology'', '''39''', 127-132.</ref>).(414 × 807 (400 KB)) - 15:31, 6 August 2014File:Figure 2.32 - Simulated 20th century Antarctic precipitation in 16 AR4 climate models.png ...precipitation averaged over the Antarctic continent by 16 IPCC AR4 coupled climate models during the 20th century.(553 × 802 (98 KB)) - 15:31, 6 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 reli3 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, sin5 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 (Chapte17 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]]. Th4 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 – 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 i12 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
File:Figure 4.8b - Linear trends of annual mean surface air temperature for 1958-2002.png ...and Walsh, J. E. 2007. A Synthesis of Antarctic Temperatures, ''Journal of Climate'', '''20''', 4096-4117.</ref>)(554 × 631 (458 KB)) - 15:30, 6 August 2014File:Figure 3.13 - Methane and d18O records covering the period 10-60 ka ago.png ...A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysics'', '''47''', RG1003, doi:10.1029/2(534 × 507 (185 KB)) - 15:30, 6 August 2014File:Figure 3.1 - Map of Antarctica showing locations of selected deep ice and sediment cores.png ...Elsevier, Amsterdam.</ref>; Barrett, 2009 for details). Further records of Antarctic geological history are found at Seymour Island (SI), James Ross Island (JRI(512 × 422 (151 KB)) - 15:30, 6 August 2014File:Figure 4.12 - Annual Antarctic snowfall accumulation anomalies.png ...han, A.J. and Bromwich, D.H. 2008. Advances in describing recent Antarctic climate variability, ''Bull. Amer. Meteorol. Soc.'', '''89''', 1295-1306.</ref>). A(529 × 276 (11 KB)) - 15:30, 6 August 2014File:Figure 3.20 - Signals of climate change in ice core records from Siple Dome and Law Dome.png ...'', '''101''', 4115-4128.</ref>). Darkened area shows the 1700-1850 AD era climate anomaly discussed in the text.(436 × 702 (289 KB)) - 15:31, 6 August 2014File:Figure 1.14 - Percentage of Antarctic macrobenthic invertebrate species of the described world fauna.png ...D.B., Wilga C.D., Seibel B.A. 2007. Climate change and invisibility of the Antarctic benthos, ''Annual Review of Ecological and Evolutionary Systems'', '''38'''(402 × 387 (40 KB)) - 15:31, 6 August 2014File:Figure 3.5 - Change in average global temperature over the last 80 million years.png ...A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysics'', '''47''', RG1003, doi:10.1029/2(435 × 524 (206 KB)) - 15:31, 6 August 2014File:Figure 3.3 - Reconstruction of mid-Cretaceous forests of Alexander Island, Antarctica.png ...ne in a Changing World. Proceedings of the 10th International Symposium on Antarctic Earth Sciences. The National Academies Press, Washington, DC, 19-27.</ref>)(420 × 276 (270 KB)) - 15:31, 6 August 2014File:Figure 4.13 - Linear trends of annual Antarctic snowfall accumulation for 1955-2004.png ...han, A.J. and Bromwich, D.H. 2008. Advances in describing recent Antarctic climate variability, ''Bull. Amer. Meteorol. Soc.'', '''89''', 1295-1306.</ref>). S(506 × 444 (98 KB)) - 15:31, 6 August 2014File:Figure 3.6 - Main climatic events of the last 65 million years in the Antarctic context.png ...A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysics'', '''47''', RG1003, doi:10.1029/2(601 × 290 (115 KB)) - 15:31, 6 August 2014File:Figure 4.11 - Annual Antarctic surface mass balance.png ...tic surface mass balance using calibrated output of a regional atmospheric climate model, ''J. Geophys. Res.'', '''111''', D11104, doi:10.10292005JD006495.</r(575 × 392 (178 KB)) - 15:31, 6 August 2014File:Figure 3.21 - Reconstructed temperatures and ice core reconstructed atmospheric circulation systems.png ...between temperature and atmospheric circulation over the last 2000 years. Climate of the Past (Discussions) http://www.copernicus.org/EGU/cp/cpd/2/327/cpd-2-(398 × 675 (293 KB)) - 15:31, 6 August 2014File:Figure 1.10 - Major currents south of 20S.png ...rtney, M.S. and Donohue, K.A. 2007. A deep cyclonic gyre in the Australian-Antarctic Basin, ''Progress in Oceanography'', '''75''', 675-750.</ref>).(601 × 589 (308 KB)) - 15:31, 6 August 2014File:Figure 4.38 - Interpolated mean annual temperature and ice shelf loss due to climate-driven retreat.png ...nsula Climate Variability: Historical and Paleoenvironmental Perspectives. Antarctic Research Series, 79, edited by E. Domack, et al., 61-68, AGU, Washington, D(360 × 552 (169 KB)) - 15:31, 6 August 2014File:Figure 3.12 - Deuterium, atmospheric CO2, CH4 and N2O from air trapped in Antarctic ice cores.png ...The Physical Science Basis. Contribution of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge.</ref>).(609 × 395 (125 KB)) - 15:31, 6 August 2014File:Figure 3.15 - Map of Antarctica showing some deep ice core sites.png ...ce cores have recently been drilled at the Detroit Plateau on the northern Antarctic Peninsula and at Titan Dome near the South Pole. Future deep ice core drill(399 × 404 (131 KB)) - 15:31, 6 August 2014File:Figure 3.19a - Antarctic and Greenland holocene climate change compared using ice core data.png ...Kreutz, K. 2004b. A 700 year record of Southern Hemisphere extra-tropical climate variability, ''Annals of Glaciology'', '''39''', 127-132.</ref>).(414 × 807 (400 KB)) - 15:31, 6 August 2014File:Figure 2.32 - Simulated 20th century Antarctic precipitation in 16 AR4 climate models.png ...precipitation averaged over the Antarctic continent by 16 IPCC AR4 coupled climate models during the 20th century.(553 × 802 (98 KB)) - 15:31, 6 August 2014File:Figure 2.37 - Simulation of a benthic succession.png ...ecosystem functioning and allow predictions of future developments of the Antarctic biosphere. This individual-based simulation of a benthic succession with a(369 × 411 (227 KB)) - 15:31, 6 August 2014File:Figure 3.14 - Climate and environmental records of Termination I.png ...ison, J.L., Werner, M. and Wolff, E. 2007. Orbital and millenial Antarctic climate variability over the past 800,000 years, ''Science'', '''317''', 793-796.</(418 × 649 (125 KB)) - 15:31, 6 August 2014File:Figure 3.7 - View of the Victoria Land coast off Cape Roberts during Oligocene and early Miocene times.png ...hown as a white filled circle. TAM = Transantarctic Mountains, EAIS = East Antarctic Ice Sheet.(479 × 471 (169 KB)) - 15:31, 6 August 2014File:Figure 2.29 - Residual of regression of bivalve species richness against sampling effort, from SOMBASE.png ...ed by ecological conditions and being of high relevance for predictions of climate change impact and natural conservation strategies.(324 × 278 (97 KB)) - 15:31, 6 August 2014- :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...t in the McMurdo Sound area (74-78ºS, 165ºE), and throughout the Antarctic Peninsula and its offshore islands (55-72ºS, 45-70ºW).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 compared16 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 reli3 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, sin5 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 (Chapte17 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]]. Th4 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 ve22 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 skil27 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 co8 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 ...Réale, D., McAdam, A.G. and Boutin, S. 2004. Keeping pace with fast climate change: can Arctic life count on evolution? Integrative Comp Biol., 44, 14016 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 e9 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, se6 KB (847 words) - 16:11, 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
- ...climate change it will be essential to use proxy records to represent how Antarctic sea ice has changed in the past. ...., Denis, D., Courty, M-A. and Ther, O. 2007 Holocene long- and short-term climate changes off Adelie Land, ''East Antarctica. Geochemistry Geophysics Geosyst24 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]]'' ...be composed of a superposition 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 [[Antarctic climate and environment history in the pre-instrumental period]]'' ...raphical coverage of high resolution records and a better understanding of climate dynamics.7 KB (1,082 words) - 15:33, 6 August 2014
- ...t places different parts in markedly different positions within the global climate system and subjects them to different environmental drivers. ...response on a centennial or millennial time scale to much older changes in climate.3 KB (475 words) - 15:33, 6 August 2014
- ...rt of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...ictions of future climate changes can only be made by using coupled global climate models (GCMs). These are also primary tools with which to simulate the past13 KB (2,051 words) - 15:33, 6 August 2014
- :''This page is part of the topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...ar regions. Palaeorecords show that profound changes in earth’s past climate have followed well-defined patterns and shifts on time scales of thousands1 KB (165 words) - 15:33, 6 August 2014
- ...nsula Climate Variability: Historical and Paleoenvironmental Perspectives, Antarctic Research Series, 79. American Geophysical Union.</ref>). ...ton, G.H., Prentice, M.L. and Burckle, L.H. 1991. Cainozoic history of the Antarctic ice sheet. In: Tingey (ed) Geology of Antarctica. Oxford University Press,22 KB (3,430 words) - 13:03, 22 August 2014