Natural variability in air–sea gas transfer efficiency of CO2
Abstract The flux of CO2 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 ob...
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| Autores principales: | , , , , , , |
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| Formato: | article |
| Lenguaje: | EN |
| Publicado: |
Nature Portfolio
2021
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| Materias: | |
| Acceso en línea: | https://doaj.org/article/8876030efbf54167bae0d984071ff7bf |
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