表面盐度上升和海冰减少:卫星揭示了南大洋的新状态
Alessandro Silvano1, Aditya Narayanan1, Rafael Catany2,3
1Ocean and Earth Science, National Oceanography Centre, University of Southampton, Southampton SO14 3ZH, United Kingdom.
概括
南大洋正在变得更加,扭转了数十年来海洋层级的降温和减弱. 这种转变与南极海冰面积的显著减少相关,可以通过卫星观察到.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 遥感 遥感 遥感 遥感
背景情况:
- 几十年来观察到的极地南洋表面清新,与气候变暖有关.
- 清新增加了海洋分层,限制了热传输和海冰融化.
- 层分也抑制了开放海洋的多形成.
研究的目的:
- 为了研究近期南洋表面盐度的变化.
- 了解这些盐度变化对海洋分层和海冰的影响.
- 评估卫星观测在监测这些动态过程中的作用.
主要方法:
- 对南洋表面盐度的卫星观测结果的分析.
- 盐度,分层和南极海冰覆盖之间的相关性分析.
- 使用遥感数据监测波利尼亚的出现.
主要成果:
- 自2015年以来,南大洋环极表面盐度明显增加.
- 上层海洋分层的减弱与南极海冰覆盖面的减少相吻合.
- 由于盐度增加,毛德升波林亚的重新出现.
结论:
- 南大洋正在从新鲜化过渡到盐化.
- 卫星监测显示了海洋条件的实时变化.
- 这种转变表明,南极海冰覆盖面持续减少的潜在转变.
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