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  • ...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) - 16:48, 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) - 16:45, 6 August 2014
  • ...f 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) - 13:25, 22 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ==Antarctic stratospheric ozone in the instrumental period==
    43 KB (6,788 words) - 17:07, 22 August 2014
  • ...f 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) - 13:38, 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 env
    13 KB (1,943 words) - 15:33, 6 August 2014
  • ...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 atmos
    7 KB (1,082 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...he ice sheet places different parts in markedly different positions within the global climate system and subjects them to different environmental drivers.
    3 KB (475 words) - 15:33, 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
  • ...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 [[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
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...tic can be determined using a number of different forms of data, including the ''in-situ'' observations, satellite infra-red imagery and ice core isotope
    30 KB (4,676 words) - 18:04, 22 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...ninsula and in Victoria Land, terrestrial habitats exist in all sectors of the continent, and both in coastal and inland locations.
    32 KB (4,651 words) - 16:17, 6 August 2014
  • :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...0300-005-0058-5.</ref>). A comprehensive field study on Antarctic krill in the Amundsen Sea has yet to be conducted.
    11 KB (1,650 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ..."Vaughan, 2006">Vaughan, D.G. 2006. Recent trends in melting conditions on the Antarctic Peninsula and their implications for ice-sheet mass balance, Arct
    40 KB (6,031 words) - 18:17, 22 August 2014
  • :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...">Rintoul, S.R. 2007. Rapid freshening of Antarctic Bottom Water formed in the Indian and Pacific Oceans, ''Geophys. Res. Lett.'', '''34''', L06606, doi:1
    14 KB (2,205 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ..., may have forestalled an anticipated increase in snowfall associated with the global trend.
    5 KB (726 words) - 15:34, 6 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...rn of flow specific to the current climate, where flow exactly compensates the spatial pattern of ice accumulation (snowfall and frost deposition) and ice
    20 KB (3,052 words) - 16:00, 6 August 2014
  • :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...r Current. Population centres drawn by eye, relative to the Commission for the Conservation of Antarctic Living Resources (CCAMLR) Survey (from Atkinson e
    28 KB (4,437 words) - 15:34, 6 August 2014
  • ...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 or
    17 KB (2,692 words) - 15:34, 6 August 2014

Page text matches

  • ...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) - 16:48, 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) - 16:45, 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 hope
    4 KB (504 words) - 17:51, 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) - 15:33, 6 August 2014
  • ...f 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) - 13:25, 22 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ==Antarctic stratospheric ozone in the instrumental period==
    43 KB (6,788 words) - 17:07, 22 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...random sample, and can &lsquo;describe&rsquo; a significant proportion of the total circulation variability.
    54 KB (8,177 words) - 13:38, 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 env
    13 KB (1,943 words) - 15:33, 6 August 2014
  • ...topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...ed over [[Antarctic climate and environment change over the next 100 years|the next 100 years]].
    3 KB (503 words) - 13:42, 22 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...ature, seasonal snow cover, wind), which interact with each other and with the ground surface characteristics (i.e. vegetation, surface microrelief).
    6 KB (847 words) - 16:11, 6 August 2014
  • ...f 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 atmosp
    20 KB (3,125 words) - 15:33, 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) - 17:17, 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) - 14:04, 22 August 2014
  • ...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 atmos
    7 KB (1,082 words) - 15:33, 6 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ...he ice sheet places different parts in markedly different positions within the global climate system and subjects them to different environmental drivers.
    3 KB (475 words) - 15:33, 6 August 2014
  • ...topic [[Antarctic climate and environment history in the pre-instrumental period]]'' ...rs. Hence studies of the past can be useful in providing insights into how the system responds and what can be expected to occur in response to future cha
    1 KB (165 words) - 15:33, 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., 2
    22 KB (3,430 words) - 13:03, 22 August 2014
  • :''This page is part of the topic [[Marine biology in the instrumental period]]'' ...l, V. 2004. Long-term decline in krill stocks and increase in salps within the Southern Ocean, ''Nature'', '''432''' (7013), 100-103.</ref>).
    15 KB (2,381 words) - 15:33, 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) - 16:16, 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) - 15:33, 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) - 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 relations
    25 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. W&auml;gele 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 h
    142 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 ecophysiologica
    38 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 re
    54 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 &ndash; 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 contradi
    8 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 sets
    5 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 revealed
    52 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 des
    10 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
  • :''This page is part of the topic [[Observations, data accuracy and tools]]'' ==The pre-satellite era==
    18 KB (2,972 words) - 17:53, 22 August 2014
  • :''This page is part of the topic [[The last million years]]'' ...Pichon, J.J. 2004. Late Qaternary sea ice history in the Indian sector of the Southern Ocean as record by diatom assemblages, ''Marine Micropaleontology'
    13 KB (2,050 words) - 15:33, 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) - 15:33, 6 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...tic can be determined using a number of different forms of data, including the ''in-situ'' observations, satellite infra-red imagery and ice core isotope
    30 KB (4,676 words) - 18:04, 22 August 2014
  • :''This page is part of the topic [[Biological responses to climate change]]'' ...gg, I.D. 2003. Long-term isolation and recent range expansion revealed for the endemic springtail Gomphiocephalus hodgsoni from southern Victoria Land, An
    21 KB (3,069 words) - 18:14, 22 August 2014
  • ...f the topic [[Antarctic climate and environment change in the instrumental period]]'' ...ninsula and in Victoria Land, terrestrial habitats exist in all sectors of the continent, and both in coastal and inland locations.
    32 KB (4,651 words) - 16:17, 6 August 2014
  • :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...0300-005-0058-5.</ref>). A comprehensive field study on Antarctic krill in the Amundsen Sea has yet to be conducted.
    11 KB (1,650 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The ice sheet in the instrumental period]]'' ..."Vaughan, 2006">Vaughan, D.G. 2006. Recent trends in melting conditions on the Antarctic Peninsula and their implications for ice-sheet mass balance, Arct
    40 KB (6,031 words) - 18:17, 22 August 2014
  • :''This page is part of the topic [[The Southern Ocean in the instrumental period]]'' ...">Rintoul, S.R. 2007. Rapid freshening of Antarctic Bottom Water formed in the Indian and Pacific Oceans, ''Geophys. Res. Lett.'', '''34''', L06606, doi:1
    14 KB (2,205 words) - 15:34, 6 August 2014
  • :''This page is part of the topic [[The Antarctic environment in the global system]]'' ...(dark) ocean, solar radiation will be absorbed rather than reflected, and the environment will warm.
    12 KB (1,933 words) - 16:38, 22 August 2014

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