Cargando…
The influence of geostrophic strain on oceanic ageostrophic motion and surface chlorophyll
Oceanic submesoscale ageostrophic processes have been progressively recognized as an important upwelling mechanism to close the nutrient budget and sustain the observed primary production of phytoplankton in the euphotic layer. Their relatively small spatio-temporal scales (of 1~10 km and a few days...
Autores principales: | Zhang, Zhengguang, Qiu, Bo, Klein, Patrice, Travis, Seth |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6599054/ https://www.ncbi.nlm.nih.gov/pubmed/31253812 http://dx.doi.org/10.1038/s41467-019-10883-w |
Ejemplares similares
-
Submesoscale transition from geostrophic flows to internal waves in the northwestern Pacific upper ocean
por: Qiu, Bo, et al.
Publicado: (2017) -
RETRACTED ARTICLE: A Complete Formula of Ocean Surface Absolute Geostrophic Current
por: Chu, Peter C.
Publicado: (2020) -
Retraction Note: A Complete Formula of Ocean Surface Absolute Geostrophic Current
por: Chu, Peter C.
Publicado: (2021) -
A 25-years dataset of ageostrophic, Ekman and Stokes surface currents in the Mediterranean Sea (AGESC-Med)
por: Morales-Márquez, Verónica, et al.
Publicado: (2023) -
Theoretical and Computational Analysis of the Thermal Quasi-Geostrophic Model
por: Crisan, D., et al.
Publicado: (2023)