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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 r
    33 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 performan
    37 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: &ldquo;How well are Antarctic organisms able to cope with daily, seasonal and longer-term environmental c
    25 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&rsquo;s former station on the Ross Ice Shelf).
    18 KB (2,723 words) - 15:33, 6 August 2014
  • ...ove &ndash; 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 [[Concludi
    14 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 &ndash; like the scale of the Antarctic Peninsula. While the spatial resolution of GCMs will increase, their capabi
    5 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 salin
    8 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> centuries
    11 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 r
    18 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 trends
    30 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 Resear
    8 KB (1,217 words) - 15:34, 6 August 2014
  • ...). Exceptions to this generalization are provided first by the continental Antarctic &lsquo;Dry Valleys&rsquo; 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
  • ...-5.</ref>). A comprehensive field study on Antarctic krill in the Amundsen Sea has yet to be conducted. ..., Jacobs, S.S., Larter, R.D. and Gohl, K. 2007. Bathymetry of the Amundsen Sea continental shelf: Implications for geology, oceanography, and glaciology,
    11 KB (1,650 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...meridional extent and fronts of the Antarctic Circumpolar Current, ''Deep-Sea Res.'', '''42''', 641-673.</ref>) and bathymetry from the General Bathymetr
    15 KB (2,479 words) - 15:34, 6 August 2014
  • ...arnes and Peck, 2008">Barnes, D.K.A. and Peck, L.S. 2008. Vulnerability of Antarctic shelf biodiversity to predicted climate change, ''Climate Research'', '''37 ...und the Antarctic Peninsula and at the sea ice margin as well as along the Antarctic Convergence (Polar Front) are the main foci of ecological climate research.
    20 KB (3,055 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...tic Peninsula and their implications for ice-sheet mass balance, Arctic, ''Antarctic and Alpine Research'', '''38''', 147-152.</ref>).
    40 KB (6,031 words) - 18:17, 22 August 2014
  • ...oul (2007<ref name="Rintoul, 2007">Rintoul, S.R. 2007. Rapid freshening of Antarctic Bottom Water formed in the Indian and Pacific Oceans, ''Geophys. Res. Lett. ...rtney, M.S. and Donohue, K.A. 2007. A deep cyclonic gyre in the Australian-Antarctic Basin, ''Progress in Oceanography'', '''75''', 675-750.</ref>).
    14 KB (2,205 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...osing large patches of bare (dark) ground, or where sea ice melts exposing ice free (dark) ocean, solar radiation will be absorbed rather than reflected,
    12 KB (1,933 words) - 16:38, 22 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...06a">Monaghan, A.J., Bromwich, D.H. and Wang, S-H. 2006a. Recent trends in Antarctic snow accumulation from Polar MM5, ''Philosophical Trans. Royal. Soc. A'', '
    5 KB (726 words) - 15:34, 6 August 2014
  • ...ne in a Changing World. Proceedings of the 10th International Symposium on Antarctic Earth Sciences. The National Academies Press, Washington, DC, 19-27.</ref>) ...ertiary times has been found on Seymour Island and Alexander Island in the Antarctic Peninsula. This demonstrates that, despite its polar position, Antarctica h
    20 KB (3,076 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...es on regional to hemispheric timescales. Second we examine changes in sea ice extent through the Holocene and how these have interacted with changing cli
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  • ...G.H., Lyons, W.B., Maasch, K.A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysics'', '''4 ...G.H., Lyons, W.B., Maasch, K.A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), ''Reviews of Geophysics'', '''4
    27 KB (4,257 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...he spatial pattern of ice accumulation (snowfall and frost deposition) and ice ablation (melting, wind erosion and calving).
    20 KB (3,052 words) - 16:00, 6 August 2014
  • ...ed, but legal and illegal fishing continues, especially for Patagonian and Antarctic Toothfish as well as for krill. ...e much more evident in the Arctic than in the Antarctic except west of the Antarctic Peninsula.
    14 KB (2,188 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...ccess of efforts to reduce the rate of greenhouse gas (GHG) emissions. The Antarctic is a long way from the main centres of population, but greenhouse gases are
    33 KB (5,155 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...f ice on global sea level. Finally we review the influence of changing sea ice distributions on climate.
    1 KB (164 words) - 15:34, 6 August 2014
  • ....J., Tarling, G.A. and Fleming, A.H. 2008. Oceanic circumpolar habitats of Antarctic krill, ''Mar. Ecol. Prog. Ser'', '''362''', 1-23.</ref>, &copy; Atkinson et ...and its wider linkages: insights revealed from models and observations, ''Antarctic Science'', '''16''', 387-400.</ref>).
    28 KB (4,437 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...meridional extent and fronts of the Antarctic Circumpolar Current, ''Deep-Sea Res.'', '''42''', 641-673.</ref>) and bathymetry from the General Bathymetr
    8 KB (1,295 words) - 16:38, 6 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...s of the heat exchange engine and the interactions of ice shelves and land ice with the ocean and atmosphere make predictions about climate change a chall
    31 KB (4,808 words) - 16:51, 22 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change over the next 100 years]]'' ...e PCO<sub>2</sub> and net CO<sub>2</sub> flux over the global oceans, Deep Sea Research, doi:10.1016/dsr2.2008.12.009.</ref>). Clearly then the way in whi
    22 KB (3,567 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ..."Rintoul et al, 2001">Rintoul, S.R., Hughes, C.W. and Olbers, D. 2001. The Antarctic Circumpolar Current system. In: Eds. G. Siedler, J. Church and J. Gould, Oc
    36 KB (5,780 words) - 16:53, 6 August 2014
  • :''This page is part of the topic [[Antarctic climate and environment change in the instrumental period]]'' ...oss Seas giving rise to subpolar gyres (Figure 1.10), the distributions of ice shelves, the zonal structure of the forcing (storm tracks) and finally the
    16 KB (2,443 words) - 15:34, 6 August 2014
  • ...i, B.S., Tison, J.L., Werner, M. and Wolff, E. 2007. Orbital and millenial Antarctic climate variability over the past 800,000 years, ''Science'', '''317''', 79 ...glaciation). Since the pioneer works of the 1960s, Greenland and Antarctic ice core records have been used to determine the magnitude of climatic and envi
    32 KB (4,956 words) - 15:34, 6 August 2014
  • ...arctic continent, and transports colder, fresher waters northward (Weddell Sea Deep and Bottom Waters, WSDW and WSBW, as well as surface waters). The tran ...ses into the formation areas and the newly formed water masses leaving the Antarctic Systems into the world oceans. However, since these transport differences a
    15 KB (2,389 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...ars ago and the concern driving much of the research of the West Antarctic ice sheet was whether such an eventuality was inevitable or even underway.
    17 KB (2,692 words) - 15:34, 6 August 2014
  • ...n a metre thick, which is why most of the large predators abandon the high Antarctic at the start of the long austral winter. ...r as a consequence of reduced food availability, despite the fact that the sea water temperature remained practically constant all year round.
    9 KB (1,434 words) - 15:34, 6 August 2014

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