623 / 2026-03-24 09:45:12
Recent pronounced warming on the Mongolian Plateau boosted by internal climate variability
区域气候变化,遥相关
Abstract Accepted
蔡晴宇 / 云南大学
Exceptionally strong summertime warming occurred over the Mongolian Plateau between 1986 and 2004, at a rate that was three times the average terrestrial warming in the Northern Hemisphere. The physical processes responsible for this extreme warming remain unclear. Here we show that the synchronous phase shift of the Interdecadal Pacific Oscillation and the Atlantic Multidecadal Oscillation contributed to this extreme Mongolian Plateau warming, which cannot be fully explained by the increasing anthropogenic CO2 alone. Pacemaker model experiments show that the Interdecadal Pacific Oscillation and Atlantic Multidecadal Oscillation excited an atmospheric wave train, resulting in an upper-level anticyclonic circulation over the Mongolian Plateau. This anticyclonic circulation increased surface warming by enhancing downward solar radiation, and the surface warming was further boosted by positive land–atmosphere feedbacks. Our results highlight the important role of internal climate variability in driving rapid regional climate change over the Mongolian Plateau.
Important Date
  • Conference Date

    Apr 25

    2026

    to

    Apr 29

    2026

  • Apr 07 2026

    Draft paper submission deadline

  • Apr 28 2026

    Registration deadline

Sponsored By
未来大气科学论坛理事会
Organized By
河海大学海洋学院
南京大学南京赫尔辛基大气与地球系统科学学院
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