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- :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...rvations and between different models. In particular, the transport of the Antarctic Circumpolar Current (ACC) through Drake Passage simulated by those models r33 KB (5,321 words) - 15:57, 22 August 2014
- ...rt of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...ace and near surface layers. Detailed studies of density currents, the sea ice field and other key regions provide further local checks on model performan37 KB (5,859 words) - 15:33, 6 August 2014
- ...d Smith, R.C. 2007. Climate change and the marine ecosystem of the western Antarctic Peninsula, ''Phil. Trans. R. Soc. B'', '''362''', 149-166.</ref>). ...sses relevant to life on Earth. Key questions include: “How well are Antarctic organisms able to cope with daily, seasonal and longer-term environmental c25 KB (3,663 words) - 15:33, 6 August 2014
- ...ount for resolving the uncertainty surrounding the future of the Antarctic ice sheet. ...snow hill is also associated with Byrd’s former station on the Ross Ice Shelf).18 KB (2,723 words) - 15:33, 6 August 2014
- ...ove – except in the case of large mammals from small islands. In the sea, though, there is not a single case of an invading NIS being successfully r ...wn S.L. 2007. Mytilus on the move: transport of an invasive bivalve to the Antarctic, ''Mar. Ecol Progr. Ser.'', '''339''', 307-310.</ref>) found that mussels (13 KB (2,063 words) - 15:33, 6 August 2014
- ...mospheric and oceanic circulation around Antarctica, and the volume of the ice sheets, interact and influence climate at a global scale. Although a great ...uplication. Other recommendations can be found in [[Future developments in Antarctic observation]], on specific observing system requirements, and in [[Concludi14 KB (2,069 words) - 16:14, 22 August 2014
- ...rt of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...rize processes that occur on a subgrid scale – like the scale of the Antarctic Peninsula. While the spatial resolution of GCMs will increase, their capabi5 KB (833 words) - 15:33, 6 August 2014
- ...d Evans, J. 2009. Mechanisms of Holocene palaeoenvironmental change in the Antarctic Peninsula region, ''The Holocene'', '''19''', 51-69.</ref>), the role of va ...story of the Antarctic Peninsula since the Last Glacial Maximum, Arctic, ''Antarctic and Alpine Research'', '''35''', 175-186.</ref>).10 KB (1,543 words) - 15:33, 6 August 2014
- ...tal Shelf. In: Eds G. Spezie and G.M.R. Manzella, Oceanography of the Ross Sea Antarctica, Springer-Verlag Italia, Milano, 3-16.</ref>). ...nd S.S. Jacobs (1994) Temporal changes in shelf water of the southern Ross Sea, ''Antarct. J. of the U.S.'', '''29'''(5), 123-124.</ref>) noted that salin8 KB (1,297 words) - 15:33, 6 August 2014
- ...erometers, infra-red and microwave sensors for sea-surface temperature and ice extent and visible-wavelength radiometers for ocean colour. Ensuring their ==Sea Surface Temperature==20 KB (3,084 words) - 15:57, 6 August 2014
- ...rt of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...arrison, 1991<ref name="Garrison, 1991">Garrison, D.L. 1991. Antarctic sea ice biota, ''Am. Zool.'', '''31''', 17-33.</ref>).18 KB (2,786 words) - 15:33, 6 August 2014
- :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...aluation of the simulation of the annual cycle of Arctic and Antarctic sea ice coverages by 11 major global climate models, J. Geophys. Res., 111, doi:10.4 KB (684 words) - 15:33, 6 August 2014
- ...only factor because the krill decline began before the retreat of the sea ice. [[Category:Antarctic biology]]2 KB (306 words) - 15:33, 6 August 2014
- ...1972">Mackintosh, N.A. 1972. Life cycle of Antarctic krill in relation to ice and water conditions, ''Discovery Reports'', '''36''', 1-94.</ref>). ...n many quarters and cannot be regarded as proof of a major decrease in sea ice extent between the 1940s and 1970s.18 KB (2,972 words) - 17:53, 22 August 2014
- ...rosta, X., Sturm, A., Armand, L. and Pichon, J.J. 2004. Late Qaternary sea ice history in the Indian sector of the Southern Ocean as record by diatom asse ==Sea ice extent==13 KB (2,050 words) - 15:33, 6 August 2014
- ==Monitoring sea level== ...mentally hostile areas to the same standard as is possible elsewhere. Most sea level measurements during the 19<sup>th</sup> and 20<sup>th</sup> centuries11 KB (1,784 words) - 15:33, 6 August 2014
- ...orison, J.H. and Nilsen, F. 2008. Revisiting heat and salt exchange at the ice-ocean interface: Ocean flux and modelling considerations, ''Journal of Geop ...Wolff, J.-O. 2004. The dynamical balance, transport and circulation of the Antarctic Circumpolar Current, ''Antarct. Sci.'', '''16''', 439-470.</ref>) for two r18 KB (2,816 words) - 15:33, 6 August 2014
- :''This page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...a, including the ''in-situ'' observations, satellite infra-red imagery and ice core isotope measurements. In order to get a reasonable estimate of trends30 KB (4,676 words) - 18:04, 22 August 2014
- ...irdle et al, 2008">Bracegirdle, T.J., Connolley, W.M. and Turner, J. 2008. Antarctic climate change over the Twenty First Century, Journal of Geophysical Resear ...irdle et al, 2008">Bracegirdle, T.J., Connolley, W.M. and Turner, J. 2008. Antarctic climate change over the Twenty First Century, Journal of Geophysical Resear8 KB (1,217 words) - 15:34, 6 August 2014
- ...). Exceptions to this generalization are provided first by the continental Antarctic ‘Dry Valleys’ of Victoria Land, providing several thousand squa ...ity as the LGM approached, leaving only continental taxa, and that the sub-Antarctic taxa have not yet returned to the lakes post LGM.21 KB (3,069 words) - 18:14, 22 August 2014