Long-lasting upper ocean temperature responses induced by intense typhoons in mid-latitude

The sea surface temperature (SST) drops rapidly when a typhoon passes over the western North Pacific, and the cold SST is known as cold wake. In general, more intense typhoons on the day of arrival cause stronger SST cooling via turbulent oceanic vertical mixing. Moreover, after intense typhoons hav...

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Detalles Bibliográficos
Autores principales: Son, Jun-Hyeok, Heo, Ki-Young, Choi, Jung-Woon, Kwon, Jae-il
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8987045/
https://www.ncbi.nlm.nih.gov/pubmed/35388123
http://dx.doi.org/10.1038/s41598-022-09833-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8987045/
https://www.ncbi.nlm.nih.gov/pubmed/35388123
http://dx.doi.org/10.1038/s41598-022-09833-2

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