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十年气候控制的循环制度在一个大边缘海洋的过渡
Lixia Zheng1, Zhongya Cai2, Jianping Gan3
1State Key Laboratory of Internet of Things for Smart City and Department of Ocean Science and Engineering, University of Macau, Macau 999078, China; Center for Ocean Research in Hong Kong and Macau, Hong Kong University of Science and Technology, Hong Kong 999077, China; Southern Marine Science and Engineering Guandong Laboratory (Zhuhai), Zhuhai 519000, China.
这是南中国海.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 海洋动力学 海洋动力学
背景情况:
- 边缘海洋连接开放的海洋和沿海系统,影响热量,盐和营养物质的运输.
- 边缘海洋的振荡行为对于海洋-大气相互作用至关重要,但人们对其了解甚少.
- 南中国海表现出独特的三层交替循环模式.
研究的目的:
- 调查1993-2008年至2009-2018年期间南海循环中的政权过渡情况.
- 了解驱动这些循环变化的动态.
- 将这些变化与气候变化联系起来,特别是太平洋十年振荡.
主要方法:
- 对历史海洋学数据的分析 (1993-2018).
- 研究表面风力强迫和太平洋交换电流的影响.
- 检查地形调制的内部垂直合器.
主要成果:
- 在2009年至2018年期间,南中国海循环中发生了明显的政权过渡,与太平洋十年振荡有关.
- 上层旋风循环在2009年后减弱,而中间层反旋风循环则加强.
- 深层循环在2009年后显著增强,由太平洋入侵和增强的垂直合推动.
结论:
- 南中国海的分层循环表现出受气候变化影响的振荡行为.
- 政权过渡是由强风,太平洋交换电流和地形驱动的.
- 这些动态在调节区域大众运输和海洋与大气相互作用方面发挥着关键作用.
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