由海浪与大气之间的相互作用调节的西部边界电流
Xiaohui Ma1,2, Zhao Jing1,2, Ping Chang1,2,3
1Physical Oceanography Laboratory/CIMST, Ocean University of China and Qingdao National Laboratory for Marine Science and Technology, Qingdao, China.
Nature
|July 29, 2016
概括
海洋与大气之间的反对于准确地模拟诸如库罗西奥延伸喷流这样的西部边界电流至关重要. 忽视这种反会削弱模拟电流,影响气候预报和极端天气事件预报.
科学领域:
- 海洋学
- 气候科学
- 大气科学
背景情况:
- 气候模型难以准确地表示海洋前线和西部边界流,如库罗西奥和湾流扩展.
- 关于西部边界电流的现有理论忽视了重要的空海相互作用,甚至在高分辨率下也导致了模型偏差.
研究的目的:
- 调查海洋中等尺度旋转和大气 (OME-A) 反在调节能量海洋流动力学的作用.
- 提高气候模型在模拟西部边界流及其相关的正面系统的准确性.
主要方法:
- 采用卷解析的气候模型模拟,主要集中在日本东部的库罗西奥延伸喷气.
- 量化了抑制OME-A反对Kuroshio扩展喷气机的强度和能源预算的影响.
主要成果:
- 抑制OME-A反导致Kuroshio延伸喷气的20-40%减弱.
- 发现OME-A反将从电流中提取的70%以上的潜在能量消散.
- 由于没有OME-A反,旋潜在的能量产生减少,导致平均电流较弱.
结论:
- 海洋中层和大气 (OME-A) 反对于充满活力的西部边界电流的动态和控制至关重要.
- 准确的OME-A反对改善气候模型对海洋前线的模拟至关重要.
- 这些发现对预测热带外风暴,极端事件和气候变化影响具有重要意义.
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