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R. O'ishi and A. Abe-Ouchi Polar amplification in the mid-Holocene derived from dynamical vegetation change with a GCM Geophysical Research Letters 38

Article first published online: 21 JUL 2011 | DOI: 10.1029/2011GL048001

Key Points

  • GCM simulated the mid-Holocene annual warming shown in proxy successfully
  • Mid-Holocene warming over land occurs mostly through vegetation feedback
  • Especially, warming occurs in all seasons but by different feedback processes

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