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河口水流结构分解及斜压M4分潮流探讨
引用本文:李谊纯,刘金贵,仉天宇,陆莎莎.河口水流结构分解及斜压M4分潮流探讨[J].海洋学报,2022,44(10):1-9.
作者姓名:李谊纯  刘金贵  仉天宇  陆莎莎
作者单位:1.广东海洋大学 海洋与气象学院 广东省近海海洋变化与灾害预警实验室,广东 湛江 524088;;2.北部湾大学 建筑工程学院,广西 钦州 535011;;3.自然资源部空间海洋遥感与应用重点实验室,北京100081;;4.广东海洋大学 广东省高等学校陆架及深远海气候、资源与环境重点实验室,广东 湛江 524088;;5.自然资源部第二海洋研究所,浙江 杭州 310012
基金项目:国家自然科学基金(41976200);广东海洋大学科研启动经费(060302032106);广东省普通高校创新团队项目(2019KCXTF021);广东省冲一流专项(080503032101-231420003)。
摘    要:河口水流是河口生态环境、河道演变、物质输运等物理过程的根本动力。由于径流、潮波、地形以及气象等因素的影响,河口水流呈现复杂的三维结构。其中既包括淡水注入形成的余流,也包括周期性的潮流、风生流、斜压流及河口非线性作用导致的流动等。为探究河口水流的组成及其潮内变化,基于瓯江口实测资料,利用主成分分析(Principal Component Analysis, PCA)法对河口水流进行分解,探讨了PCA法对河口水流的分解性能及斜压分潮流的高频特征。研究认为,PCA法在河口水流结构研究中既可采用原始数据操作亦可用标准化的数据进行计算。PCA法可分解出斜压成分(河口重力环流型结构),但不能将正压成分(径流和潮流)分开,径流和潮流二者综合作用的结果体现在主成分的得分之中。主成分的取舍应根据水流结构和累计解释方差综合判断,不宜仅依据累计解释方差。河口斜压流动具有明显的高频特征,近似呈1/4日分潮的周期。

关 键 词:斜压    PCA    M4分潮    瓯江口    河口重力环流
收稿时间:2022-04-13
修稿时间:2022-06-27

Flow structure decomposition and baroclinic M4 constituent current exploration in estuarine zone
Li Yichun,Liu Jingui,Zhang Tianyu,Lu Shasha.Flow structure decomposition and baroclinic M4 constituent current exploration in estuarine zone[J].Acta Oceanologica Sinica (in Chinese),2022,44(10):1-9.
Authors:Li Yichun  Liu Jingui  Zhang Tianyu  Lu Shasha
Institution:1. Guangdong Key Laboratory for Coastal Ocean Variation and Disaster Prediction, College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China;;2. College of Civil Engineering and Architecture, Beibu Gulf University, Qinzhou 535011, China;;3. Key Laboratory of Space Ocean Remote Sensing and Application, Ministry of Natural Resources, Beijing 100081, China;;4. Key Laboratory of Climate, Resources and Environment in Continental Shelf Sea and Deep Sea of Department of Education of Guangdong Province, Guangdong Ocean University, Zhanjiang 524088, China;;5. Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
Abstract:Estuarine flow is the fundamental driving of physical processes such as estuarine ecological environment, river evolution and material transport. Due to the runoff, tide, topography and meteorology, the estuarine flow presents a complex three-dimensional structure, including not only the residual flow induced by fresh water injection, but also the periodical tidal current, wind-driven flow, baroclinic flow and the residual flow caused by estuarine nonlinearity. In order to explore the composition and intra-tidal variation of estuarine flow, based on the field data in the Oujiang River Estuary, the estuarine flow is decomposed by principal component analysis (PCA) method, and the decomposition performance of PCA method for estuarine flow and high-frequency characteristics of baroclinic overtide are deeply discussed. The results show that PCA method can operate original data or standardized data in the study of estuarine flow structure. PCA method can decompose baroclinic components (estuarine gravitational circulation structure), but cannot separate barotropic components (runoff and tidal current). The coupled effect of runoff and tidal current is reflected in the score of principal components. The filter of principal components should employ conjoint judgment of flow structure and cumulative interpretation variance, rather than only cumulative interpretation variance. The estuarine baroclinic flow has clearly high-frequency characteristics, which approximates quarter-diurnal.
Keywords:baroclinic  PCA  M4<  sub> constituent  Oujiang River Estuary  estuarine gravitational circulation
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