Glider observations of interleaving layers beneath the Kuroshio primary velocity core east of Taiwan and analyses of underlying dynamics

Submesoscale interleaving layers are caused by lateral intrusions of dissimilar water masses in frontal zones, which are significant processes in shaping physical, biogeochemical, and ecological parameters in the ocean. Possible interleaving layers were sometimes observed by ship-based conductivity-...

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Detalles Bibliográficos
Autores principales: Jan, Sen, Wang, Shih-Hong, Yang, Kai-Chieh, Yang, Yiing Jang, Chang, Ming-Huei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6684527/
https://www.ncbi.nlm.nih.gov/pubmed/31388070
http://dx.doi.org/10.1038/s41598-019-47912-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6684527/
https://www.ncbi.nlm.nih.gov/pubmed/31388070
http://dx.doi.org/10.1038/s41598-019-47912-z

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