近几十年来北大西洋北部的稀释
Ruth Curry1, Cecilie Mauritzen
1Woods Hole Oceanographic Institution (WHOI), Woods Hole, MA 02543, USA. rcurry@whoi.edu
概括
自20世纪60年代以来,大规模的淡水添加到北大西洋,正在刷新关键地区. 这一大量的淡水流入可能会在下一个世纪影响大西洋南部翻转循环.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 水文学的水文学
背景情况:
- 海洋盐度是淡水流量的关键指标.
- 北大西洋在全球海洋循环模式中起着至关重要的作用.
研究的目的:
- 量化进入北欧海和亚极盆地的淡水输入量和时间.
- 评估观察到的新鲜化对大西洋南部翻转循环的潜在影响.
主要方法:
- 从20世纪60年代中期到90年代中期的历史盐度数据的分析.
- 根据盐度变化估计淡水量和输入速度.
主要成果:
- 据估计,19000 +/- 5000立方公里额外的淡水进入了北欧海和亚极盆地在1965年至1995年之间.
- 大约有1万立方千米的淡水进入了20世纪60年代末的每年2000立方千米的速度.
- 观察到的淡水积累表明,达到关键的清新值需要一个世纪的时间.
结论:
- 自20世纪中叶以来,北大西洋北部发生了显著的新鲜化.
- 淡水输入的速度,特别是在20世纪60年代末,是相当大的.
- 这些变化可能对大西洋南部翻转循环的稳定性产生长期影响.
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