Cargando…
Latitude-dependent finescale turbulent shear generations in the Pacific tropical-extratropical upper ocean
Turbulent mixing, which is critically important for the equilibrium of ocean circulation, is controlled by finescale turbulent shear (S(2)) of oceanic flows through shear instability. Although the relationship between S(2) and mixing is well understood, the latitude-dependent generation processes of...
Autores principales: | Zhang, Zhiwei, Qiu, Bo, Tian, Jiwei, Zhao, Wei, Huang, Xiaodong |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2018
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6173738/ https://www.ncbi.nlm.nih.gov/pubmed/30291235 http://dx.doi.org/10.1038/s41467-018-06260-8 |
Ejemplares similares
-
Trends and variability of the atmosphere–ocean turbulent heat flux in the extratropical Southern Hemisphere
por: Herman, Agnieszka
Publicado: (2015) -
Steady State Ocean Response to Wind Forcing in Extratropical Frontal Regions
por: Cronin, Meghan F., et al.
Publicado: (2016) -
Erratum: Steady State Ocean Response to Wind Forcing in Extratropical Frontal Regions
por: Cronin, Meghan F., et al.
Publicado: (2016) -
Eastern equatorial Pacific cold tongue evolution since the late Miocene linked to extratropical climate
por: Liu, Jingjing, et al.
Publicado: (2019) -
Salinity fronts in the tropical Pacific Ocean
por: Kao, Hsun-Ying, et al.
Publicado: (2015)