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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...

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Detalles Bibliográficos
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