Cargando…
Increasing deep-water overflow from the Pacific into the South China Sea revealed by mooring observations
Cold and dense water from the North Pacific Ocean that spills through the Luzon Strait, the only deep conduit between the South China Sea (SCS) and the Pacific Ocean, renews deep-water mass, modulates hydrographic and biogeochemical cycles, and drives abyssal and overturning circulations in the SCS....
Autores principales: | Zhou, Chun, Xiao, Xin, Zhao, Wei, Yang, Jiayan, Huang, Xiaodong, Guan, Shoude, Zhang, Zhiwei, Tian, Jiwei |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2023
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10085979/ https://www.ncbi.nlm.nih.gov/pubmed/37037814 http://dx.doi.org/10.1038/s41467-023-37767-4 |
Ejemplares similares
-
An extreme internal solitary wave event observed in the northern South China Sea
por: Huang, Xiaodong, et al.
Publicado: (2016) -
On the identification of internal solitary waves from moored observations in the northern South China Sea
por: Gong, Qinglong, et al.
Publicado: (2023) -
Tropical Meridional Overturning Circulation Observed by Subsurface Moorings in the Western Pacific
por: Song, Lina, et al.
Publicado: (2018) -
Sources and upstream pathways of the densest overflow water in the Nordic Seas
por: Huang, Jie, et al.
Publicado: (2020) -
Mooring observed intraseasonal oscillations in the central South China Sea during summer monsoon season
por: Jan, Sen, et al.
Publicado: (2021)