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自2016年以来,观察到的机制激活了最近的亚极北大西洋变暖
Léon Chafik1,2, N Penny Holliday2, Sheldon Bacon2
1Department of Meteorology, Stockholm University, Stockholm, Sweden.
概括
最近东部亚极北大西洋 (SPNA) 的变暖与西深边界密度的增加有关. 这增强了热传输,推动了自2016年以来观察到的变暖趋势.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 地球系统科学 地球系统科学
背景情况:
- 亚极北大西洋循环对于全球气候变化至关重要.
- 了解该地区最近的变暖趋势对于气候预测至关重要.
研究的目的:
- 调查自2016年以来推动东部亚极北大西洋近期变暖的机制.
- 确定海洋循环变化在区域气候变化中的作用.
主要方法:
- 分析来自亚极北大西洋的观测数据.
- 在西部边界调查密度异常.
- 评估北大西洋电流和热传输的变化.
主要成果:
- 自大约2016年以来,观察到东方SPNA的西部边界密度增加.
- 这种密度增加与受北大西洋振荡影响的增强浮力强迫有关.
- 深密度异常向南传播,加强北大西洋流和南部热传输.
结论:
- 东部SPNA最近 (2016年以来) 的变暖阶段主要是由增强的热量流入驱动的.
- 这种涌入是由深西部边界密度的变化促进的,这是海洋循环的关键组成部分.
- 这些发现强调了大气模式和海洋热传输在区域气候变化中的相互联系.
关键词:
大西洋南部翻转的循环.更多相关视频
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