Eurasia’s transition from colder winters to hotter summers driven by North Atlantic air–sea interaction and Arctic sea ice anomalies
ID:56 View Protection:ATTENDEE Updated Time:2026-03-20 13:23:00 Hits:170 Extended type 2

Start Time:2026-04-26 13:30(Asia/Shanghai)

Duration:20min

Session:S1-14 专题1.14 极地与中低纬气候系统相互作用 » F5专题1.14 极地与中低纬气候系统相互作用

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Abstract
Extreme cold winters and hot summers over Eurasia are intensifying under global warming, pos
ing substantial risks to agriculture, ecosystems, and human health. Here, we show that a colder
winter tends to be followed by a hotter summer over Eurasia. This winter-summer extreme tem
perature reversal is linked to the phase switch of the Arctic oscillation (AO) from winter to sum
mer, which is driven by the North Atlantic air–sea interaction and Arctic sea ice-atmosphere coup
ling. Specifically, a negative AO in winter weakens high-latitude westerlies, causing cold extremes
over Eurasia. Negative AO also induces a tripolar sea surface temperature anomaly in the North
Atlantic that persists into the following summer and triggers positive AO-like atmospheric anom
alies, leading to a hotter summer across Eurasia. Moreover, winter atmospheric anomalies reduce
the Barents–Kara sea ice through horizontal moisture transport. This sea ice loss persists into
summer and contributes to the formation of positive AO-like atmospheric anomalies. These pro
cesses establish a cross-seasonal transition from extreme cold winters to extreme hot summers over
Eurasia, offering new insight into the prediction of summer extreme events.
Keywords
极端事件、北极海冰、北大西洋海气相互作用
Speaker
陈尚锋
研究员 中国科学院大气物理研究所

Submission Author
陈尚锋 中国科学院大气物理研究所
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Important Date
  • Conference Date

    Apr 25

    2026

    to

    Apr 29

    2026

  • Apr 07 2026

    Draft paper submission deadline

  • Jun 17 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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