Natural variability in air–sea gas transfer efficiency of CO(2)

The flux of CO(2) between the atmosphere and the ocean is often estimated as the air–sea gas concentration difference multiplied by the gas transfer velocity (K(660)). The first order driver for K(660) over the ocean is wind through its influence on near surface hydrodynamics. However, field observa...

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Detalles Bibliográficos
Autores principales: Yang, Mingxi, Smyth, Timothy J., Kitidis, Vassilis, Brown, Ian J., Wohl, Charel, Yelland, Margaret J., Bell, Thomas G.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8245487/
https://www.ncbi.nlm.nih.gov/pubmed/34193883
http://dx.doi.org/10.1038/s41598-021-92947-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8245487/
https://www.ncbi.nlm.nih.gov/pubmed/34193883
http://dx.doi.org/10.1038/s41598-021-92947-w

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