Timing and amplitude biases in modeled dissolved inorganic carbon and temperature produce out of phase pCO2 and CO2 fluxes: A Southern Ocean case study
Timing and amplitude biases in modeled dissolved inorganic carbon and temperature produce out of phase pCO2 and CO2 fluxes: A Southern Ocean case study
Seth M Bushinsky1, Lionel Arteaga2, Andrea J Fassbender3, Judith Hauck4, Matthew R Mazloff5, Ivana Cerovecki6, Peter Landschützer7, Christian Rödenbeck8, Christopher Danek9, Anastasia Romanou10, Paul Lerner10, Alison R Gray11 and Sarah Schlunegger12, (1)University of Hawaii at Manoa, Department of Oceanography, Honolulu, United States, (2)Princeton University, Princeton, NJ, United States, (3)NOAA Pacific Marine Environmental Laboratory, Seattle, United States, (4)Alfred Wegener Institute Helmholtz-Center for Polar and Marine Research, Bremerhaven, Germany, (5)Scripps Institution of Oceanography, UCSD, La Jolla, United States, (6)Scripps Institution of Oceanography, San Diego, United States, (7)Flanders Marine Institute (VLIZ), Ostend, Belgium, (8)Max Planck Institute for Biogeochemistry, Jena, Germany, (9)University of Bonn, Meteorological Institute, Bonn, Germany, (10)NASA Goddard Institute for Space Studies, New York, NY, United States, (11)University of Washington, School of Oceanography, Seattle, United States, (12)Princeton University, Atmospheric and Oceanic Sciences, Princeton, NJ, United States