Numerical Modeling of Tidal Phenomena of Penzhina Bay

IF 1.3 4区 地球科学 Q4 OCEANOGRAPHY Oceanology Pub Date : 2024-01-08 DOI:10.1134/s0001437023060140
D. R. Shpachuk, O. V. Sokolov, A. N. Bugaets
{"title":"Numerical Modeling of Tidal Phenomena of Penzhina Bay","authors":"D. R. Shpachuk, O. V. Sokolov, A. N. Bugaets","doi":"10.1134/s0001437023060140","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>In this study, the <i>Delft3D-Flow</i> hydrodynamic model was used to determine the characteristics of the main tidal waves and currents in Penzhina Bay (Sea of Okhotsk, Russia). The initial and boundary conditions are set according to the TPXO9 model data, and the salinity and water temperature for each model layer are set based on reanalysis data of the HYCOM ocean general circulation model, with a time step of 3 h. The European Center for Medium-Range Weather Forecasts (ECMWF) ERA-5 reanalysis was used as meteoforcing. Modeling was performed for the ice-free period from May to September 2005. Maps of cotidal lines, tidal ellipses, and reversibility coefficients for the main tidal waves were constructed: semidiurnal wave M2 and diurnal wave K1. The model was verified by comparing the published and calculated harmonic components for nine sea level monitoring points located in Penzhina Bay. Conformance evaluation generally shows a high degree of consistency between the model and reference data. The values of the determination coefficient <i>R</i><sup>2</sup> between the series formed by the model and published harmonic components range from 0.96 to 0.99. According to the magnitude of relative errors, the modeling results are divided into two consistency categories: high (1.48–2.14%) and satisfactory (2.93–4.27%). Spatial distribution patterns for the values of relative errors were not found. A certain inconsistency in the results is presumably due to the time discretization of the observation time support and the short sea level monitoring data series used to calculate the published harmonic components for Penzhina Bay.</p>","PeriodicalId":54692,"journal":{"name":"Oceanology","volume":null,"pages":null},"PeriodicalIF":1.3000,"publicationDate":"2024-01-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Oceanology","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1134/s0001437023060140","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"OCEANOGRAPHY","Score":null,"Total":0}
引用次数: 0

Abstract

In this study, the Delft3D-Flow hydrodynamic model was used to determine the characteristics of the main tidal waves and currents in Penzhina Bay (Sea of Okhotsk, Russia). The initial and boundary conditions are set according to the TPXO9 model data, and the salinity and water temperature for each model layer are set based on reanalysis data of the HYCOM ocean general circulation model, with a time step of 3 h. The European Center for Medium-Range Weather Forecasts (ECMWF) ERA-5 reanalysis was used as meteoforcing. Modeling was performed for the ice-free period from May to September 2005. Maps of cotidal lines, tidal ellipses, and reversibility coefficients for the main tidal waves were constructed: semidiurnal wave M2 and diurnal wave K1. The model was verified by comparing the published and calculated harmonic components for nine sea level monitoring points located in Penzhina Bay. Conformance evaluation generally shows a high degree of consistency between the model and reference data. The values of the determination coefficient R2 between the series formed by the model and published harmonic components range from 0.96 to 0.99. According to the magnitude of relative errors, the modeling results are divided into two consistency categories: high (1.48–2.14%) and satisfactory (2.93–4.27%). Spatial distribution patterns for the values of relative errors were not found. A certain inconsistency in the results is presumably due to the time discretization of the observation time support and the short sea level monitoring data series used to calculate the published harmonic components for Penzhina Bay.

Abstract Image

查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
笔架山湾潮汐现象的数值模拟
摘要 本研究采用 Delft3D-Flow 流体动力模型确定了奔日那湾(俄罗斯鄂霍次克海)主要潮汐波和潮流的特征。初始条件和边界条件根据 TPXO9 模型数据设定,各模型层的盐度和水温根据 HYCOM 海洋总环流模型的再分析数据设定,时间步长为 3 小时。建模时间为 2005 年 5 月至 9 月的无冰期。绘制了潮汐线图、潮汐椭圆图和主要潮汐波的可逆系数图:半日波 M2 和昼波 K1。通过比较位于笔架山湾的九个海平面监测点的已公布谐波分量和计算谐波分量,对模型进行了验证。一致性评估结果表明,模型与参考数据之间具有很高的一致性。由模型形成的序列与公布的谐波分量之间的判定系数 R2 值在 0.96 至 0.99 之间。根据相对误差的大小,模型结果分为两个一致性类别:高(1.48-2.14%)和满意(2.93-4.27%)。没有发现相对误差值的空间分布规律。结果的不一致性可能是由于观测时间支持的时间离散化以及用于计算已公布的奔子栏海湾谐波分量的海平面监测数据序列较短所致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
Oceanology
Oceanology 地学-海洋学
CiteScore
2.00
自引率
20.00%
发文量
83
审稿时长
6-12 weeks
期刊介绍: Oceanology, founded in 1961, is the leading journal in all areas of the marine sciences. It publishes original papers in all fields of theoretical and experimental research in physical, chemical, biological, geological, and technical oceanology. The journal also offers reviews and information about conferences, symposia, cruises, and other events of interest to the oceanographic community.
期刊最新文献
Monitoring of a Seasonal Local Aggregation of Beluga Whales Delphinapterus leucas Based on Presumed Identification “Contact Calls”: a Pilot Study Phytoplankton of the Ob Estuary (Kara Sea) in the Season Preceding Winter Features of the Distribution of Black Sea Ichthyoplankton in Conditions of Activation of Atmospheric Processes in the Summer Hydrological Season of 2021 Preliminary Data on the Depth Effect on the Nematode Community in the East Siberian Sea Meiobenthos of the Côn Đảo Islands (Vietnam): Differences in the Structure of Taxocenes of Reef Flats and Mangroves
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1