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The effects of historical ozone changes on Southern Ocean heat uptake and storage

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Abstract

Atmospheric ozone concentrations have dramatically changed in the last five decades of past century. Herein we explore the effects of historical ozone changes that include stratospheric ozone depletion on Southern Ocean heat uptake and storage, by comparing CESM1 large ensemble simulations with fixed-ozone experiment. During 1958–2005, the ozone changes contribute to about 50% of poleward intensification of the Southern Hemisphere westerly winds in historical simulations, which intensifies the Deacon Cell and residual meridional overturning circulation, thus contributing to heat redistribution in the Southern Ocean. Heat budget analysis shows that, in response to historical ozone changes, heat is taken up between 50 and 58 °S mainly through changes in sensible heat flux, shortwave radiation flux, and the flux due to seasonal sea ice formation and melt. A major part of the absorbed heat, however, is redistributed equatorward primarily through Eulerian mean ocean heat transport such that ocean heat storage peaks at lower latitudes, around 44 °S. The ozone-induced interior warming contributes to about 22% of the historical Southern Ocean warming over 1958–2005. Poleward of 62 °S where a subsurface temperature inversion occurs, shoaling isopycnals lead to warming and salinification in the upper ocean. To the north of 50 °S, the deep-reaching warming and freshening that correspond to the ocean heat storage maximum are primarily set by the deepening of isopycnals. The large-scale patterns of isopycnal shoaling (deepening) at high (middle) latitudes are consistent with the overlying negative (positive) wind stress curl anomalies related to the poleward intensification of westerly winds, suggesting that the wind changes play an important role in the Southern Ocean heat redistribution under the ozone forcing.

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Acknowledgements

This work was supported by grants to WL by the Regents’ Faculty Fellowship, and by the Sloan Research Fellowship. KL and XZ were funded by the Centre for Southern Hemisphere Oceans Research (CSHOR), jointly funded by the Qingdao National Laboratory for Marine Science and Technology (QNLM, China) and the Commonwealth Scientific and Industrial Research Organisation (CSIRO, Australia). The CESM1 Large Ensemble and CESM1 Fixed Ozone Ensemble data are available at Climate Date Gateway at NCAR on the page https://www.earthsystemgrid.org/. The ERA-20CM reanalysis is available at https://www.ecmwf.int/en/forecasts/datasets/browse-reanalysis-datasets. The JRA-55 reanalysis is available at https://jra.kishou.go.jp/JRA-55/index_en.html. The NCEP/NCAR-R1 reanalysis is available at https://psl.noaa.gov/data/gridded/data.ncep.reanalysis.html. The EN4.2.1 data are available at http://www.metoffice.gov.uk/hadobs/en4/index.html. The IAP data are available at http://159.226.119.60/cheng/. The GECCO3 data are available at http://icdc.cen.uni-hamburg.de/en/gecco3.html. The ORAS4 data are available at https://icdc.cen.uni-hamburg.de/daten/reanalysis-ocean/easy-init-ocean/ecmwf-ocean-reanalysis-system-4-oras4.html.

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Li, S., Liu, W., Lyu, K. et al. The effects of historical ozone changes on Southern Ocean heat uptake and storage. Clim Dyn 57, 2269–2285 (2021). https://doi.org/10.1007/s00382-021-05803-y

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  • DOI: https://doi.org/10.1007/s00382-021-05803-y

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