Direct observation of the oceanic CO(2) increase revisited
We show, from recent data obtained at specimen North Pacific stations, that the fossil fuel CO(2) signal is strongly present in the upper 400 m, and that we may consider areal extrapolations from geochemical surveys to determine the magnitude of ocean fossil fuel CO(2) uptake. The debate surrounding...
I tiakina i:
| I whakaputaina i: | Proc Natl Acad Sci U S A |
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| Ngā kaituhi matua: | , , |
| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
National Academy of Sciences
1997
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| Ngā marau: | |
| Urunga tuihono: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC33732/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/11607738/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.94.16.8308 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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