于宇君,孟静,陈旭,杨华

• 1:中国海洋大学物理海洋教育部重点实验室
• 2:中国海洋大学海洋学实验教学中心
• 3:中国海洋大学信息科学与工程学院

摘要(Abstract)：

内潮是海洋能量级串中重要环节,对维持海洋背景层结及大尺度环流结构起着重要的作用。本文设计了粗糙地形内潮导致混合的实验方案,对内潮混合机制进行了探讨。根据混合机理将流场分为三个区域:底边界层区、近底边界层区及远离边界层区。利用PIV及ADV观测内潮流场中断面的流速,计算并对比了两者的无量纲流速振幅、雷诺剪切应力及湍耗散率。对比结果良好,实验方案可用于内潮混合的实验研究。

关键词(KeyWords)： 内潮;混合;湍耗散率;粒子图像测速技术(PIV);声谱多普勒流速仪(ADV)

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金仪器专项(61727806);国家自然科学基金项目(41476001;41276008)资助~~

作者(Author): 于宇君,孟静,陈旭,杨华

DOI: 10.16441/j.cnki.hdxb.20170368

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