亚等尺度是全球海洋表面边界层的重要流源
Jihai Dong1,2, Baylor Fox-Kemper3, Jacob O Wenegrat4
1School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing, China. jihai_dong@nuist.edu.cn.
Nature communications
|November 5, 2024
概括
亚质量级海洋前沿在海洋边界层的动动能中起着显著的作用,挑战了传统观点. 这一发现影响了气候模型和我们对海洋能源和碳循环的理解.
科学领域:
- * 海洋学 海洋学
- * 气候科学 气候科学
- * 流体动力学 流体动力学
背景情况:
- *海洋表面边界层对气候至关重要,影响能源和碳循环.
- * 准确的气候模型取决于了解海洋流.
- * 传统的流源包括波浪,风和对流.
研究的目的:
- * 调查海洋前沿的亚尺度现象作为流能量来源的作用.
- * 量化亚尺度地质剪切产生的海洋边界层动动能预算的贡献.
主要方法:
- * 应用一个非维的动动能动能预算方程.
- *分析海洋边界层内的流,重点关注亚介质尺度前线.
主要成果:
- * 海洋前沿的亚大尺度地质剪切是动荡能量的重要来源,特别是在远离海面的地方.
- *这种贡献可以占冬季总消散量的34%和夏季在深度中部的17%.
- * 尽管在空间和时间上是间歇性的,但能量贡献是显著的.
结论:
- *以前对海洋边界层流的理解从根本上来说是缺陷的.
- * 在气候模型中必须考虑前沿的亚介质规模过程.
- *需要重新评估观察尺度,模型分辨率和参数化.
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