EGU22-13273
https://doi.org/10.5194/egusphere-egu22-13273
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Transient response of surface-forced water mass transformation over the Southern Ocean and its connection to overturning and ventilation

Jan-Erik Tesdal1,2, Graeme A. MacGilchrist1,2, Rebecca. L. Beadling1,2, John P. Krasting2, Stephen M. Griffies1,2, and Paul J. Durack3
Jan-Erik Tesdal et al.
  • 1Program in Atmospheric and Oceanic Sciences, Princeton University, United States
  • 2Geophysical Fluid Dynamics Laboratory, National Oceanic and Atmospheric Administration, United States
  • 3Program for Climate Model Diagnosis and Intercomparison, Lawrence Livermore National Laboratory

The water mass transformation (WMT) framework provides a useful perspective on interior ocean circulation because it combines the influence of surface forcing and diapycnal mixing with overturning. Observational analyses, as well as the majority of ocean model diagnostics, only adequately resolve surface-forced transformation of water masses and rely on inference or rough approximations to quantify the effect of the interior transformation term due to mixing. Here we characterize the connection between surface-forced WMT and meridional overturning of the Southern Ocean in two state-of-the-art GFDL coupled climate models. We assess the mean state of the system as well as the transient response to changes in surface forcing. For the latter, we analyze a set of idealized perturbation experiments in which changes in Antarctic ice sheet melting and Southern Ocean wind stress are imposed. Assessment of the mean state in the two climate models is consistent with previous studies that identified overturning as a balance between surface and interior WMT, with the surface component being the dominant term. However, the perturbation runs in both models demonstrate important differences in the response of surface WMT and meridional overturning. Changes in overturning are consistent with surface WMT but are muted in terms of intensity, location, and the density at which they occur. This points to a crucial role for interior WMT associated with mixing, as well as changes in water mass volumes, which are important terms in characterizing anticipated shifts in overturning and ventilation in the Southern Ocean in response to anthropogenic forcing.

How to cite: Tesdal, J.-E., MacGilchrist, G. A., Beadling, R. L., Krasting, J. P., Griffies, S. M., and Durack, P. J.: Transient response of surface-forced water mass transformation over the Southern Ocean and its connection to overturning and ventilation, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-13273, https://doi.org/10.5194/egusphere-egu22-13273, 2022.

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