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- ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...ost and physical realism. This is especially true for ocean models because the computational cost is always high, and can be hundreds of times that of a c37 KB (5,859 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...-surface temperature and ice extent and visible-wavelength radiometers for ocean colour. Ensuring their continuity is of paramount importance.20 KB (3,084 words) - 14:57, 6 August 2014
- :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...uantification of such processes is a prerequisite for successful modelling the large scale conditions.18 KB (2,816 words) - 14:33, 6 August 2014
- ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...Observed CO<sub>2</sub> emissions over the last 25 years as compared with the different IPCC emission scenarios (Raupach et al., 2007<ref name="Raupach e22 KB (3,567 words) - 14:34, 6 August 2014
- ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...d Duffy, 2000">Caldeira, K. and Duffy, P.B. 2000. The role of the Southern Ocean in uptake and storage of anthropogenic carbon dioxide, ''Science'', '''287'36 KB (5,780 words) - 15:53, 6 August 2014
- ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...nd finally the different hydrographic conditions in the northward adjacent ocean basins.16 KB (2,443 words) - 14:34, 6 August 2014
Page text matches
- ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...n-uniform due to the influence of ocean currents and spatial variations in ocean warming. Global warming from increasing greenhouse gas concentrations is a16 KB (2,491 words) - 12:16, 22 August 2014
- ...itions across the Southern Ocean, ocean conditions, the sea ice extent and the terrestrial and marine biology. ...emainder of the Nineteenth Century and it was not possible to venture into the inhospitable interior of Antarctica.3 KB (501 words) - 15:48, 6 August 2014
- ...e changes observed in recent decades. This is particularly the case in the ocean where we have few long time series of physical measurements and remarkably ...ls to derive various estimates of how temperature may change over land and ocean.5 KB (788 words) - 15:49, 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) - 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 hope4 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
- ...is page is part of 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
- ...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) - 16:07, 22 August 2014
- ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...random sample, and can ‘describe’ 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 [[Atmospheric change over the next 100 years]]'' ...istribution of sea ice, and the seasonal to interannual variability of the Southern Hemisphere.29 KB (4,462 words) - 16:11, 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 env13 KB (1,943 words) - 14:33, 6 August 2014
- ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...nd Harris, 2005">Beaman, R.J. and Harris, P.T. 2005. Bioregionalization of the George V Shelf, East Antarctica, ''Cont. Shelf Res.'', '''25''', 1657-1691.8 KB (1,225 words) - 14:33, 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 depe16 KB (2,488 words) - 14:33, 6 August 2014
- ...page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...name="Peck, 2005">Peck, L.S. 2005. Prospects for survival in the Southern Ocean: vulnerability of benthic species to temperature change, ''Antarctic Sci.''4 KB (557 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...and bound to be upset by rapid changes such as those that are occurring at the present time.9 KB (1,315 words) - 14:33, 6 August 2014
- ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...en Broeke, M.R., Reijmer, C.H. and Van Meijgaard, E. 2006. Reassessment of the Antarctic surface mass balance using calibrated output of a regional atmosp20 KB (3,125 words) - 14:33, 6 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
- ...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 atmos7 KB (1,082 words) - 14:33, 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) - 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., 222 KB (3,430 words) - 12:03, 22 August 2014
- :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...ong-term decline in krill stocks and increase in salps within the Southern Ocean, ''Nature'', '''432''' (7013), 100-103.</ref>).15 KB (2,381 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...ed increasingly in recent decades and this trend is certain to continue in the future.7 KB (1,040 words) - 15:16, 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
- :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...ated with the climate regime can be interpreted as major driving forces on the large scale biogeography of marine water breathing animals. These relations25 KB (3,817 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...d Asper, 2007">Smith, W. and Asper, V.A. 2007. New Ways to Collect Data in the Antarctic, EOS, Transactions American Geophysical Union, 88, no. 48, 525.</17 KB (2,672 words) - 14:50, 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 h142 KB (22,142 words) - 15:25, 6 August 2014
- ...is page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...is small compared to what it was following the LGM Transition and through the Holocene.8 KB (1,342 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...ouse gases may reduce the value of Antarctica and the surrounding Southern Ocean for research on evolutionary and ecophysiological processes and as an ideal38 KB (5,770 words) - 14:33, 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 re54 KB (8,173 words) - 14:33, 6 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 both9 KB (1,386 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Biota of the Antarctic]]'' ...rs of the Antarctic shelf comparable to classic evolutionary sites such as the Galapagos.43 KB (6,450 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...tionally to inform future models and enhance our understanding of Southern Ocean microbial ecology.2 KB (305 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...atic stations. A further boost to the observing network has taken place in the International Polar Year of 2007 – 2008.59 KB (9,046 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...shortcomings, so their results have to be considered with as much care as the ones derived from observations alone. Indeed, some models throw up contradi8 KB (1,343 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...e and increasingly, biological studies. In this section we examine some of the major classes of models used in Antarctic studies.2 KB (322 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
- ...tained from satellite systems that have become increasingly important over the last couple of decades. ...ng to be employed in biology – a trend that seems set to continue in the future.2 KB (307 words) - 15:44, 6 August 2014
- :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...arctic environment, such as meteorology, solar-terrestrial interactions in the Earth’s outer atmosphere (known as ‘geospace’), coastal s5 KB (752 words) - 14:09, 22 August 2014
- :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...ues below the mean; grey areas: no representative data. This example shows the high spatial heterogeneity obviously shaped by ecological conditions and be23 KB (3,516 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Observations, data accuracy and tools]]'' ...tion about the processes that operate to change the Antarctic environment. The combination of fieldwork, aircraft, and satellite measurements has revealed52 KB (8,045 words) - 14:43, 22 August 2014
- ...page is part 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) - 14:57, 22 August 2014
- ...s part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...ost and physical realism. This is especially true for ocean models because the computational cost is always high, and can be hundreds of times that of a c37 KB (5,859 words) - 14:33, 6 August 2014
- :''This page is part of the topic [[Marine biology over the next 100 years]]'' ...s, D.K.A. and Smith, R.C. 2007. Climate change and the marine ecosystem of the western Antarctic Peninsula, ''Phil. Trans. R. Soc. B'', '''362''', 149-16625 KB (3,663 words) - 14:33, 6 August 2014