Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints

No abstract is available for this paper.

• Publication year

  2006

• Venue

  Climate Dynamics

• Publication date

  2006-05-19

• Fields of study

  Geology, Physics, Environmental Science

• Identifiers
  DOI 10.1007/S00382-005-0081-9
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

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  2005influential reference
• Holocene climate evolution in the high-latitude Southern Hemisphere simulated by a coupled atmosphere-sea ice-ocean-vegetation model

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  2005influential reference
• Impacts of a Warming Arctic: Arctic Climate Impact Assessment

  2004cited by this paper
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  2004cited by this paper
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  2004influential reference
• GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE

  2004influential reference
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  2004cited by this paper
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  2004cited by this paper
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  2004cited by this paper
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  2004cited by this paper
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  2003influential reference
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  2003cited by this paper
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  2003cited by this paper
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  2002cited by this paper
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  2001cited by this paper
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  2001cited by this paper
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  2000influential reference
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  2000cited by this paper
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  1999cited by this paper
• Monsoon changes for 6000 years ago: Results of 18 simulations from the Paleoclimate Modeling Intercomparison Project (PMIP)

  1999cited by this paper
• Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

  1999cited by this paper
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  1999cited by this paper
• Altitude dependence of the ice sheet surface climate

  1999cited by this paper
• Synergistic feedbacks from ocean and vegetation on the African Monsoon response to Mid‐Holocene insolation

  1999cited by this paper
• Synchronous climate changes in antarctica and the north atlantic

  1998cited by this paper
• GCM simulations of the Last Glacial Maximum surface climate of Greenland and Antarctica

  1998cited by this paper
• Past temperatures directly from the greenland ice sheet

  1998cited by this paper
• Impact of parameterizations on simulated winter mid‐Holocene and Last Glacial Maximum climatic changes in the northern hemisphere

  1998cited by this paper
• Detection of temperature and sea-ice-extent changes in the Antarctic and Southern Ocean, 1949-96

  1998cited by this paper
• Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition

  1997cited by this paper
• Sensitivity of paleoclimate simulation results to season definitions

  1997cited by this paper
• The Role of sea ice in 2×CO2 climate model sensitivity: Part II: Hemispheric dependencies

  1997cited by this paper
• Effect of vegetation on an ice-age climate model simulation

  1997cited by this paper
• Air content along the Greenland Ice Core Project core: A record of surface climatic parameters and elevation

  1997cited by this paper
• Cool tropical temperatures shift the global δ18O‐T relationship: An explanation for the ice core δ18O ‐ borehole thermometry conflict?

  1997cited by this paper
• The δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability

  1997cited by this paper
• GCM analysis of local influences on ice core δ signals

  1997cited by this paper
• The climate of Europe 6000 years ago

  1996cited by this paper
• Large Arctic Temperature Change at the Wisconsin-Holocene Glacial Transition

  1995cited by this paper
• Greenland palaeotemperatures derived from GRIP bore hole temperature and ice core isotope profiles

  1995cited by this paper
• Ice Age Paleotopography

  1994influential reference
• New precipitation and accumulation maps for Greenland

  1991cited by this paper
• The ice-core record: climate sensitivity and future greenhouse warming

  1990cited by this paper
• Vostok ice core: climatic response to CO2 and orbital forcing changes over the last climatic cycle

  1987cited by this paper
• A comparison of climate model sensitivity with data from the last glacial maximum.

  1985cited by this paper
• Seasonal reconstructions of the earth's surface at the last glacial maximum

  1981cited by this paper
• Long-term variations of daily insolation and Quaternary climatic changes

  1978cited by this paper
• Variation in the mean deuterium content of precipitations in Antarctica

  1969cited by this paper

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