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A method of constructing a dynamic chart depth model for coastal areas

The depth is important for vessel navigation at sea. Currently, most vessels use electronic navigation charts to navigate at sea. In coastal areas, especially close to shallow water areas, the dynamic change of the water level is very important to safe navigation. Ships calculate the change of water...

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Autores principales: Guan, Minglei, Tian, Chenyang, Wang, Bin, Ji, Fangzheng, Sun, Rui, Yu, Song, Wang, Chongping, Wang, Qi, Wang, Jingzhe, Zhang, Wei, Zhang, Dejin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: PeerJ Inc. 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10363341/
https://www.ncbi.nlm.nih.gov/pubmed/37489122
http://dx.doi.org/10.7717/peerj.15616
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author Guan, Minglei
Tian, Chenyang
Wang, Bin
Ji, Fangzheng
Sun, Rui
Yu, Song
Wang, Chongping
Wang, Qi
Wang, Jingzhe
Zhang, Wei
Zhang, Dejin
author_facet Guan, Minglei
Tian, Chenyang
Wang, Bin
Ji, Fangzheng
Sun, Rui
Yu, Song
Wang, Chongping
Wang, Qi
Wang, Jingzhe
Zhang, Wei
Zhang, Dejin
author_sort Guan, Minglei
collection PubMed
description The depth is important for vessel navigation at sea. Currently, most vessels use electronic navigation charts to navigate at sea. In coastal areas, especially close to shallow water areas, the dynamic change of the water level is very important to safe navigation. Ships calculate the change of water level by using up-to-date tide tables, to obtain the dynamic water depth in the channels. However, the depth caused by the tide and non-tidal components may reach several meters in some seas, causing the dynamic depth below the safety depth, which can easily lead to grounding of vessels stranding accidents. The channel is regularly dredged to achieve navigational depth. Without regular dredging, the offshore non-channel area becomes the common area of ship grounding. The dynamic chart depth model studied in this article can provide real-time depth, which serves the ships navigation in the non-channel. The model incorporates the chart depth and the dynamic water levels on the same reference datum. The chart depth is from the electronic navigational chart depth. The dynamic water levels are constructed by the simulated tidal levels and continuous series of nontidal residual. We then designed a deviation correction method to reduce the discrepancy of the simulated tidal level with the actual water level, including datum offset correction and residual water level correction. Finally, by merging the revised dynamic water levels with the electronic navigational chart depth, we obtained the dynamic chart depth model of the study region.
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spelling pubmed-103633412023-07-24 A method of constructing a dynamic chart depth model for coastal areas Guan, Minglei Tian, Chenyang Wang, Bin Ji, Fangzheng Sun, Rui Yu, Song Wang, Chongping Wang, Qi Wang, Jingzhe Zhang, Wei Zhang, Dejin PeerJ Statistics The depth is important for vessel navigation at sea. Currently, most vessels use electronic navigation charts to navigate at sea. In coastal areas, especially close to shallow water areas, the dynamic change of the water level is very important to safe navigation. Ships calculate the change of water level by using up-to-date tide tables, to obtain the dynamic water depth in the channels. However, the depth caused by the tide and non-tidal components may reach several meters in some seas, causing the dynamic depth below the safety depth, which can easily lead to grounding of vessels stranding accidents. The channel is regularly dredged to achieve navigational depth. Without regular dredging, the offshore non-channel area becomes the common area of ship grounding. The dynamic chart depth model studied in this article can provide real-time depth, which serves the ships navigation in the non-channel. The model incorporates the chart depth and the dynamic water levels on the same reference datum. The chart depth is from the electronic navigational chart depth. The dynamic water levels are constructed by the simulated tidal levels and continuous series of nontidal residual. We then designed a deviation correction method to reduce the discrepancy of the simulated tidal level with the actual water level, including datum offset correction and residual water level correction. Finally, by merging the revised dynamic water levels with the electronic navigational chart depth, we obtained the dynamic chart depth model of the study region. PeerJ Inc. 2023-07-20 /pmc/articles/PMC10363341/ /pubmed/37489122 http://dx.doi.org/10.7717/peerj.15616 Text en ©2023 Guan et al. https://creativecommons.org/licenses/by/4.0/This is an open access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/) , which permits unrestricted use, distribution, reproduction and adaptation in any medium and for any purpose provided that it is properly attributed. For attribution, the original author(s), title, publication source (PeerJ) and either DOI or URL of the article must be cited.
spellingShingle Statistics
Guan, Minglei
Tian, Chenyang
Wang, Bin
Ji, Fangzheng
Sun, Rui
Yu, Song
Wang, Chongping
Wang, Qi
Wang, Jingzhe
Zhang, Wei
Zhang, Dejin
A method of constructing a dynamic chart depth model for coastal areas
title A method of constructing a dynamic chart depth model for coastal areas
title_full A method of constructing a dynamic chart depth model for coastal areas
title_fullStr A method of constructing a dynamic chart depth model for coastal areas
title_full_unstemmed A method of constructing a dynamic chart depth model for coastal areas
title_short A method of constructing a dynamic chart depth model for coastal areas
title_sort method of constructing a dynamic chart depth model for coastal areas
topic Statistics
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10363341/
https://www.ncbi.nlm.nih.gov/pubmed/37489122
http://dx.doi.org/10.7717/peerj.15616
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