High‐Frequency Correlations Between Winds and pCO2 Change the California Coastal Upwelling System From a CO2 Sink to a Source
Abstract Net sea‐air CO2 flux can be calculated from observations of seawater and atmosphere partial pressure of CO2 (pCO2) and estimates of the gas transfer velocity. Typically, these quantities are calculated at a monthly resolution, which misses potentially important high‐frequency temporal varia...
I tiakina i:
| Ngā kaituhi matua: | , , , , , |
|---|---|
| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Wiley
2025-07-01
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| Rangatū: | Geophysical Research Letters |
| Ngā marau: | |
| Urunga tuihono: | https://doi.org/10.1029/2025GL115470 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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