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- ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...orcing (storm tracks) and finally the different hydrographic conditions in the northward adjacent ocean basins.16 KB (2,443 words) - 15:34, 6 August 2014
- :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...and involving ocean, atmosphere and cryosphere and a major contribution to the deep meridional overturning cell (Figure 1.9).15 KB (2,389 words) - 15:34, 6 August 2014
- :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...glacial, 125,000 years ago and the concern driving much of the research of the West Antarctic ice sheet was whether such an eventuality was inevitable or17 KB (2,692 words) - 15:34, 6 August 2014
Page text matches
- :''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
- :''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) - 17:41, 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) - 17:43, 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) - 15:33, 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) - 15:33, 6 August 2014
- :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...2002">Wiencke, C. and Clayton, M.N. 2002. Antarctic Seaweeds, (Synopses of the Antarctic Benthos. Ed.: J. W. Wägele and J. Sieg ; Vol. 9), Ruggell :11 KB (1,587 words) - 15:33, 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) - 18:27, 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) - 16:25, 6 August 2014
- ...f 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) - 15:33, 6 August 2014
- :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...c contaminants and greenhouse gases may reduce the value of Antarctica and the surrounding Southern Ocean for research on evolutionary and ecophysiologica38 KB (5,770 words) - 15:33, 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) - 15:33, 6 August 2014
- ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' #[[The open ocean system in the instrumental period]]657 B (84 words) - 15:33, 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) - 15:33, 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) - 15:33, 6 August 2014
- :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...oastal sea ice conditions, and sea level. These observations have produced instrumental records that are in many cases 50 years long, providing important data sets5 KB (752 words) - 15:09, 22 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) - 15:43, 22 August 2014
- ...ill major gaps in our knowledge and many areas where we require additional instrumental data gathering and model development. ...limate change on geological time scales. In addition, scattered throughout the text there are many statements about additional research requirements.14 KB (2,069 words) - 16:14, 22 August 2014
- :''This page is part of the topic [[The Holocene]]'' ...the Antarctic Peninsula region, ''The Holocene'', '''19''', 51-69.</ref>), the role of various forcing mechanisms in regional climate change is poorly des10 KB (1,543 words) - 15:33, 6 August 2014
- :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...Continental Shelf. In: Eds G. Spezie and G.M.R. Manzella, Oceanography of the Ross Sea Antarctica, Springer-Verlag Italia, Milano, 3-16.</ref>).8 KB (1,297 words) - 15:33, 6 August 2014
- :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...t be the only factor because the krill decline began before the retreat of the sea ice.2 KB (306 words) - 15:33, 6 August 2014
