The ocean-internal processes (biology, transport) that add/remove dissolved inorganic carbon to/from the mixed-layer and thus cause anomalies in sea-air CO2 fluxes, simultaneously also remove/add dissolved oxygen, leading to anomalies in the sea-air oxygen exchange and finally to tiny but detectable variations in the atmospheric oxygen abundance. Thus, regular atmospheric oxygen measurements contain information on ocean-internal biogeochemical processes (Keeling and Shertz, 1992).
Using an atmospheric inversion technique similar to the Jena CO2 inversion, sea-air oxygen exchanges have been estimated from atmospheric O2/N2 measurements (Rödenbeck et al., 2008). In order to eliminate the influence of land processes on atmospheric oxygen abundance, the tracer Atmospheric Potential Oxygen (APO) has been used (Stephens et al., 1998).
| Run ID / version | Period of validity | Set-up | Atm. sites | Status Date of release | Estimated APO Fluxes | Atmosph. APO Fields |
|---|---|---|---|---|---|---|
| apo94_v2022 | 1994-2021 | Std. inv. | 5 (apo94v2022) | current 2023-04-28 | Download... | |
| apo97_v2022 | 1997-2021 | Std. inv. | 7 (apo97v2022) | current 2023-04-28 | Download... | |
| apo99_v2022 | 1999-2021 | Std. inv. | 9 (apo99v2022) | current 2023-04-28 | Download... | |
| apo99X_v2022 | 1999-2021 | Std. inv. | 11 (apo99Xv2022) | current 2023-04-28 | Download... | |
| apo99XS_v2022 | 2002-2021 | Std. inv. | 12 (apo99XSv2022) | current 2023-04-28 | Download... | Download... |