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OAS accession Detail for 0301544
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accessions_id: | 0301544 | archive |
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Title: | Revised estimates of ocean-atmosphere CO2 flux accounting for near-surface temperature and salinity deviations from 1985-01-01 to 2019-12-31 (NCEI Accession 0301544) |
Abstract: | The ocean is a sink for ~25% of the atmospheric CO2 emitted by human activities, an amount in excess of 2 petagrams of carbon per year (PgC yr−1). Time-resolved estimates of global ocean-atmosphere CO2 flux provide an important constraint on the global carbon budget. However, previous estimates of this flux, derived from surface ocean CO2 concentrations, have not corrected the data for temperature gradients between the surface and sampling at a few meters depth, or for the effect of the cool ocean surface skin. Here we calculate a time history of ocean-atmosphere CO2 fluxes from 1992 to 2018, corrected for these effects. These increase the calculated net flux into the oceans significantly. |
Date received: | 20250204 |
Start date: | 19850101 |
End date: | 20191231 |
Seanames: | World-Wide Distribution |
West boundary: | -180 |
East boundary: | 180 |
North boundary: | 90 |
South boundary: | -90 |
Observation types: | chemical, derived products |
Instrument types: | carbon dioxide (CO2) gas analyzer |
Datatypes: | AIR-SEA FLUX - PARTIAL PRESSURE (OR FUGACITY) OF CARBON DIOXIDE |
Submitter: | Watson, Andrew J. |
Submitting institution: | University of Exeter |
Collecting institutions: | University of Exeter |
Contributing projects: | OCADS |
Platforms: | |
Number of observations: | |
Supplementary information: | This data package (Submission ID: BH3KR9U1E) was acquired by NCEI from the Scientific Data Integration System (SDIS) at the NOAA Pacific Marine Environmental Laboratory (PMEL) in accordance with the archival submission agreement between NCEI and PMEL. For description of the method see Watson et al, Nature. Communications vol11 art no 4422, (2020) |
Availability date: | |
Metadata version: | 4 |
Keydate: | 2025-02-04 21:35:21+00 |
Editdate: | 2025-02-05 16:29:19+00 |