引用本文:[点击复制]
[点击复制]
【打印本页】 【在线阅读全文】【下载PDF全文】 查看/发表评论下载PDF阅读器关闭

←前一篇|后一篇→

过刊浏览    高级检索

本文已被:浏览 5342次   下载 4925 本文二维码信息
码上扫一扫!
辽河口岸线变化对潮不对称影响的研究
李庆臻,张学庆,赵杨,于金珍
0
(中国海洋大学环境科学与工程学院, 山东 青岛 266100)
摘要:
受河口地形等因素的影响,潮汐潮流会出现涨落潮不对称现象,这种不对称对河口物质输运过程具有重要的影响.本研究采用流通量偏度和水位不对称度的统计方法研究辽河口岸线变化对潮波变形的影响.结果表明,辽河口潮汐潮流不对称性表现为涨潮主导型,岸线变化导致涨潮历时延长,落潮历时减小,不对称度缩减了0.007~0.071;岸线变化导致涨潮流速减小,落潮流速增大,流通量偏度缩减了0.000~0.248,岸线变化对潮流不对称的影响程度比对潮汐影响的程度大.
关键词:  海洋水文学  岸线变化  数值模拟  潮汐不对称  流通量偏度  辽河口
DOI:10.3969/J.ISSN.2095-4972.2018.03.005
基金项目:国家重点基础研究发展计划资助项目(2015CB453301)
Modeling tidal asymmetry response to shoreline change in Liaohe Estuary
LI Qing-zhen,ZHANG Xue-qing,ZHAO Yang,YU Jin-zhen
(Key Laboratory of Marine Environment and Ecology, Ministry of Education, Ocean University of China, Qingdao 266100, China)
Abstract:
Due to the influence of estuary topography and other factors, the asymmetry of tide and tidal current often occurs. To succinctly quantify the asymmetry phenomenon in the estuary, the statistical flood-ebb asymmetry and volume flux skewness are referred. Such features are significantly known to be important role on the mass transport. It is evident that it becomes flood-dominant in Liaohe Estuary after tides and tidal current asymmetry occurs. More interestingly, it is a localized feature that the flood duration prolonged and the ebb duration reduced after shoreline change. The amplitude of its scale decreased between 0.007 and 0.071. The volume flux skewness reduced varying from 0.000 to 0.248 which demonstrates a decreasing in flood current velocity and an increasing in ebb velocity. In general, the influence of shoreline change on tidal current asymmetry is greater than tidal elevation asymmetry.
Key words:  marine hydrology  shoreline change  numerical simulation  tidal asymmetry  flux skewness  Liaohe Estuary

用微信扫一扫

用微信扫一扫