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自20世纪50年代以来,南大洋的变暖
1Scripps Institution of Oceanography and Department of Mechanical and Aerospace Engineering, University of California San Diego, La Jolla, CA 92093-0230, USA. sgille@ucsd.edu
概括
南大洋中部深度温度在20世纪50年代至80年代间大幅上升. 这种由自主拉格朗日循环探测器浮标记录的变暖速度比全球海洋变暖快,并且集中在南极环极流中.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 南大洋动力学 南大洋动力学
背景情况:
- 历史上的水文数据为南大洋温度提供了基线.
- 自主拉格朗循环探测器 (ALACE) 浮动器为海洋学变化提供了新的见解.
研究的目的:
- 为了分析南大洋中部深度温度趋势.
- 为了将南大洋的变暖速度与全球平均值进行比较.
主要方法:
- 使用来自ALACE浮动器的温度记录,部署在700米至1100米的深度之间.
- 将1990年代的ALACE数据与20世纪50年代至80年代的历史水文测量数据进行比较.
主要成果:
- 南大洋中部深度温度显示,从20世纪50年代到20世纪80年代,气温上升趋势为0.17摄氏度.
- 观测到的南大洋的变暖速度比全球海洋平均水平快.
- 在南极环极流中,温度变化最为明显.
结论:
- 南大洋在中深处正在经历加速变暖.
- 南极环极流的变暖速度与大气温度的增加相当.
- 这些发现凸显了南大洋对气候变化的敏感性.
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