...
  • 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Estuarine Coastal and Shelf Science >Intermittent large amplitude internal waves observed in Port Susan, Puget Sound
【24h】

Intermittent large amplitude internal waves observed in Port Susan, Puget Sound

机译：在普吉特海湾苏珊港观察到间歇性大振幅内波

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

A previously unreported internal tidal bore, which evolves into solitary internal wave packets, was observed in Port Susan, Puget Sound, and the timing, speed, and amplitude of the waves were measured by CID and visual observation. Acoustic Doppler current profiler (ADCP) measurements were attempted, but unsuccessful. The waves appear to be generated with the ebb flow along the tidal flats of the Stillaguamish River, and the speed and width of the resulting waves can be predicted from second-order KdV theory. Their eventual dissipation may contribute significantly to surface mixing locally, particularly in comparison with the local dissipation due to the tides. Visually the waves appear in fair weather as a strong foam front, which is less visible the farther they propagate. (C) 2017 Elsevier Ltd. All rights reserved.
机译：在普吉特海湾苏珊港观察到以前未报告的内潮汐波，演变成单独的内波波包，并通过CID和目测观察了波的时间，速度和振幅。尝试进行声学多普勒电流分析仪（ADCP）测量，但未成功。这些波似乎是沿着斯蒂拉瓜米什河的潮汐带的退潮而产生的，由此产生的波的速度和宽度可以根据二阶KdV理论进行预测。它们的最终耗散可能显着地促进了表面的局部混合，特别是与潮汐引起的局部耗散相比。从视觉上看，在晴朗的天气中，海浪以坚固的泡沫锋面出现，传播越远，就越不可见。 （C）2017 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱：kefu@zhangqiaokeyan.com

京公网安备：11010802029741号 ICP备案号：京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有

  • 客服微信

  • 服务号