Aug 26, 2021

Southern Ocean Air-Sea Carbon Fluxes from Aircraft Observations: Modeling Datasets


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Version: 1.0

The Southern Ocean plays an important role in determining atmospheric CO2, yet estimates of air-sea CO2 flux for the region diverge widely. We constrain Southern Ocean air-sea CO2 exchange by relating fluxes to horizontal and vertical CO2 gradients in atmospheric transport models and then apply atmospheric observations of these gradients to estimate fluxes. Aircraft-based measurements of the vertical atmospheric CO2 gradient provide robust flux constraints. We find an annual-mean flux of –0.55±0.23 Pg C yr–1 (net uptake) south of 45°S during 2009–2018. This is consistent with the mean of atmospheric-inversion estimates and surface-ocean pCO2-based products, but our data indicate stronger annual-mean uptake than suggested by recent interpretations of profiling-float observations.

DOI
https://doi.org/10.5065/fepv-0z52
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GCMD Science Keywords
  • Atmosphere > Atmospheric Chemistry > Carbon And Hydrocarbon Compounds > Carbon Dioxide
  • Oceans > Ocean Chemistry > Carbon Dioxide
GCMD Platform Types
  • Other > Models > Cesm > Ncar Community Earth System Model
File Media Types
  • application/gzip
  • text/plain
Support Contact
Matthew Long
UCAR/NCAR - Climate and Global Dynamics Laboratory
mclong@ucar.edu

Data Curator
GDEX Curator
UCAR/NCAR - GDEX
datahelp@ucar.edu

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Creative Commons Attribution 4.0 International License.
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None
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Version History
1.0
Authors
Long, Matthew
Stephens, Britton B.
McKain, Kathryn
Sweeney, Colm
Chandra, Naveen
Chevallier, Frederic
Luijkx, Ingrid T.
Patra, Prabir
Peters, Wouter
Rödenbeck, Christian
Publisher
UCAR/NCAR - GDEX

Suggested Citation
Long, Matthew, Stephens, Britton B., McKain, Kathryn, Sweeney, Colm, Chandra, Naveen, Chevallier, Frederic, Luijkx, Ingrid T., Patra, Prabir, Peters, Wouter, Rödenbeck, Christian. (2021). Southern Ocean Air-Sea Carbon Fluxes from Aircraft Observations: Modeling Datasets. Version 1.0. UCAR/NCAR - GDEX. https://doi.org/10.5065/fepv-0z52. Accessed 02 May 2024.
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