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北极反气旋循环的人类加剧
Zhongfang Liu1, Camille Risi2, Francis Codron3
1State Key Laboratory of Marine Geology, Tongji University, Shanghai, China.
Science advances
|February 26, 2025
概括
温室气体主要推动巴伦茨-卡拉海 (BKS) 反气旋循环的加强,导致放大气候变暖和海冰流失. 这种积极的反循环影响北极气候及其他地区.
科学领域:
- 大气科学 大气科学
- 气候科学是气候科学.
- 北极研究研究研究北极研究
背景情况:
- 巴伦茨-卡拉海 (BKS) 在过去的四十年中经历了冬季反气旋循环的加强.
- 这种循环变化与放大局部变暖,海冰损失和欧亚冷却有关.
- 在BKS中这种大气循环趋势的驱动因素仍然不清楚.
研究的目的:
- 确定观察到BKS冬季抗气旋循环强化的主要驱动因素.
- 研究将大气循环变化与北极变暖和海冰流失联系在一起的机制.
- 为了解北极大气对人为气候变化的反应提供一个框架.
主要方法:
- 对大气循环趋势的归因分析.
- 气候建模以隔离温室气体和气溶的影响.
- 研究变暖,海冰和大气循环之间的反机制.
主要成果:
- 人为温室气体被确定为主要的驱动因素 (约. 86%的趋势),而人为气溶起到了次要的作用.
- 这两种强迫都导致BKS中低热层变暖的放大,加上海冰的大量损失.
- 放大变暖导致地势高度增加,增强抗气旋循环,并创造一个积极的反循环.
结论:
- 人为强迫,主要是温室气体,是加强BCS抗气旋循环的原因.
- 一个积极的反循环,涉及放大变暖和海冰损失,加强了循环变化.
- 这些发现提供了对北极气候动态的见解,并对北极环境产生了更广泛的影响.
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