Published December 31, 2024 | Version 2024-12-31
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Exploring the formation of ocean current and the underlying hydrology

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DOI:10.58473/JAES0011      Retrieval from official database: www.crossref.org

All rights reserved. This upload includes formally published article (updated version), pre-print, software and dataset. 

2024.Copyrights Certificate Registered by Brock Chain Technology: Brock Chain ID (1520f70e74c0cf00fdc74c84211072ec32f31d6f79942438b0666e4b04de87a8). Registered Time:   2024-12-25 08:13.

The formally published serials is the printing <Journal of Astronomy and Earth Sciences (ISSN2958-4043)>, and the serials NO. is the month/year when the materials is accessible on this website, authorized by publisher; 正式发表的期刊是印刷版《天文与地球科学杂志》(ISSN2958-4043),期刊期号为文章内容在本网站上网年/月,出版人许可自行正式发表。

Abstract: The first part of this article comprehensively reviews the relevant theories on ocean hydrology, with substantial discussion of new theories revealing the boundary layer formation process; Then representative case studies are conducted and based on the existing data that have been published, it is to re-edit and re-analyze the results with regards to the strong-wind driven current, sea-air interactions, various ocean circulation modes, ocean pollution transport and mitigation; Thirdly, this article builds up a numerical model to simulate the formation of boundary layers.

Key words: Ocean hydrology, Ocean current, Boundary layer, Ocean circulation, Ocean pollution.    

This research project is formally registered via Open Science Framework (OSF) Registry, USA. Project DOI: https://doi.org/10.17605/OSF.IO/PUQMT ; The finalization of this project is registered via OSF with DOI: https://doi.org/10.17605/OSF.IO/VHZK8

This registered research project is indexed in BASE: Link

Scilit Database: Link       PlumX: Link     Researchgate (Cited-By): Link    DataCite Commons (Metadata Download): Link

Web of Science: https://publons.com/wos-op/publon/72172733/

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Journal article: 10.58473/JBS0024 (DOI)
Other: 10.5281/zenodo.14213870 (DOI)