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  • ...be used for predictions of the future. Instead, coupled Chemistry-Climate Models are used. Those whose results are described below vary in their skill in re '''Table 5.1''' Models whose results appear in Figures 5.11, 5.12 and 5.13; * bromine chemistry no
    27 KB (4,305 words) - 16:22, 6 August 2014
  • The availability of gridded data from numerical weather prediction (NWP) models and reanalyses allows entirely automated methods to be used that can provid
    54 KB (8,177 words) - 13:38, 22 August 2014
  • ...ulti-model study, ''Ocean Sci.'', '''1''', 81-95.</ref>), although in some models a peak at around 7 years is observed (Marshall et al., 2007<ref name="Marsh ...Twentieth century simulation of the Southern Hemisphere climate in coupled models. Part 1: Large scale circulation variability, ''Clim. Dyn.'', '''26''', 217
    29 KB (4,462 words) - 17:11, 22 August 2014
  • ...40-year trends similar to those observed are reproduced in global climate models forced by a combination of ozone depletion, and increasing greenhouse gas c ...and of the consequences for inland ice sheet flow are needed to test such models. To attribute the glaciological changes in the Amundsen Sea sector to a par
    13 KB (1,943 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...rona antarctica (Myctophidae, Pisces) in Kerguelen by generalized additive models and geographic information systems, ''Polar Biol.'', '''30''', 951-959.</re
    8 KB (1,225 words) - 15:33, 6 August 2014
  • ...ntarctic surface mass balance and systematic biases in general circulation models, ''J. Geophys. Res.'', '''106''', 20653-20664.</ref>), van Lipzig et al. (2 ...meterizations of polar cloud microphysics and precipitation in atmospheric models (Guo et al., 2003<ref name="Guo et al, 2003">Guo, Z., Bromwich, D.H. and Ca
    20 KB (3,125 words) - 15:33, 6 August 2014
  • ...is debated. In order to improve the incorporation of sea ice into computer models of future climate change it will be essential to use proxy records to repre
    24 KB (3,785 words) - 17:17, 22 August 2014
  • ...radically revise their view of ice sheet sensitivity to climate. Existing models, based primarily on earlier views of the essential governing dynamics of ic ...et, Science, 320, No. 5877, 781-783.</ref>). It must be borne in mind that models disagree over many other details of atmospheric climate change in Antarctic
    26 KB (4,124 words) - 14:04, 22 August 2014
  • ...at have survived through glacial cycles also challenges existing ice sheet models where most of the available habitats are covered at the LGM.
    7 KB (1,082 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...past and present-day climates. Simulation of present day climates by these models provides a way of rigorously testing their ability to reproduce reality. Su
    13 KB (2,051 words) - 15:33, 6 August 2014
  • ...elf. While the Antarctic Peninsula Ice Sheet (APIS) has, according to some models, been a relatively minor (1-2 m) contributor to post-LGM sea level rise, it
    22 KB (3,430 words) - 13:03, 22 August 2014
  • ...004. Southern Ocean sea ice and its wider linkages: insights revealed from models and observations, ''Antarctic Science'', '''16''', 387-400.</ref>). Food we
    15 KB (2,381 words) - 15:33, 6 August 2014
  • ...ched in 2009. Ocean salinity observations will be important to studies and models of the circulation of the Southern Ocean and the role of sea ice. These obs ...hese data are essential for understanding ocean processes and as inputs to models for forecasting future change.
    7 KB (1,040 words) - 16:16, 22 August 2014
  • ...sea ice cover, sea level rise and rising terrestrial carbon storage. Other models have identified the importance of on and off states of the southern overtur
    35 KB (5,415 words) - 15:33, 6 August 2014
  • ...in percent derived with Modern Analog Techniques and Generalized Additive Models. Signature legend: (1) concomitant occurrence of cold-water indicator diato
    17 KB (2,705 words) - 17:43, 22 August 2014
  • :''This page is part of the topic [[Models of the physical and biological environment of the Antarctic]]'' ...tion of subglacial sediments. A recent overview of the status of Antarctic models is provided by Huybrechts (2004<ref name="Huybrechts, 2004">Huybrechts, P.
    33 KB (5,053 words) - 15:33, 6 August 2014
  • ...thermal ectotherms. In: Davison W, Williams CW (Eds) Antarctic Ecosystems: Models for a Wider Understanding, Caxton Press, Christchurch, New Zealand, 109-122 ...al growth rates of Antractic krill (''Euphausia superba''): II: Predictive models based on food, temperature, body length, sex, and maturity stage, ''Limnolo
    25 KB (3,817 words) - 15:33, 6 August 2014
  • ...s their consequences for the biosphere, and shows how the latest numerical models project changes into the future, taking into account human interference in ..., which is sensitive to changes in atmospheric and oceanic conditions. The models can be weighted according to their skill in simulating modern conditions.</
    48 KB (7,673 words) - 18:27, 22 August 2014
  • ...DRILLing (ANDRILL) project geological records, a feature also simulated by models (Pollard and DeConto, 2009<ref name="Pollard and DeConto, 2009">Pollard, D. ...) points to significant loss of Greenland and Antarctic ice. While climate models are able to capture the patterns of the orbital-driven warming of the Arcti
    142 KB (22,142 words) - 16:25, 6 August 2014
  • ...pointed out by Milne (2009<ref name="Milne, 2009">Milne, G.A. 2009. Using models to inform the field community: Far-field sea level data applications, PAGES
    8 KB (1,342 words) - 15:33, 6 August 2014

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