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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...
Autores principales: | Son, Jun-Hyeok, Heo, Ki-Young, Choi, Jung-Woon, Kwon, Jae-il |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
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Materias: | |
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 |
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