最近秋季在北极东部的海冰消失,夏季亚太振荡增强了亚太振荡
Botao Zhou1,2, Ziyi Song3,4, Zhicong Yin3,4
1Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change, Nanjing University of Information Science and Technology, Nanjing, China. zhoubt@nuist.edu.cn.
Nature communications
|March 30, 2024
概括
亚太振荡 (APO) 推动了北极海冰的消失. 一个积极的APO阶段使北大西洋变暖,导致湿度和温度增加,加速秋季海冰融化.
科学领域:
- 北极气候动态 北极气候动态
- 大气中的远程连接.
- 海冰的变化性是不同的.
背景情况:
- 北极海冰正在迅速减少,原因是人为强迫和内部气候变化.
- 内部气候变化在北极海冰流失中的具体作用尚不清楚.
- 亚太振荡 (APO) 是一种影响温度模式的大气模式.
研究的目的:
- 调查亚太振荡 (APO) 作为秋季北极东部海冰变化的驱动因素.
- 阐明将APO与北极海冰融化的机制.
主要方法:
- 对大气和海洋数据的分析.
- 调查APO和海面温度之间的远程连接.
- 检查巴伦茨-卡拉拉普特夫海和东西伯利亚海的异常天气模式.
主要成果:
- 阳性夏季APO阶段与北大西洋中度海面温度升温相关.
- 这种变暖影响大气循环,在巴伦茨-卡拉-拉普特夫海上产生反气旋异常,在东西伯利亚海上产生气旋异常.
- 这些变化增强了北极东部的水分传输,湿度,长波辐射和表面空气温度,促进了海冰的融化.
结论:
- 亚太振荡 (APO) 被认为是秋季北极东部海冰变化的关键驱动因素.
- 最近趋向于夏季积极的APO阶段的趋势有助于加速秋季海冰的消失.
- 了解内部变化,就像APO一样,对于预测北极海冰变化至关重要.
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