Articles | Volume 14, issue 5
https://doi.org/10.5194/esd-14-1085-2023
https://doi.org/10.5194/esd-14-1085-2023
Research article
 | 
25 Oct 2023
Research article |  | 25 Oct 2023

A quantitative assessment of air–sea heat flux trends from ERA5 since 1950 in the North Atlantic basin

Johannes Mayer, Leopold Haimberger, and Michael Mayer

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Cited articles

Baehr, J., Haak, H., Alderson, S., Cunningham, S. A., Jungclaus, J. H., and Marotzke, J.: Timely Detection of Changes in the Meridional Overturning Circulation at 26 N in the Atlantic, J. Clim., 20, 5827–5841, https://doi.org/10.1175/2007JCLI1686.1, 2007. a
Baker, J. A., Renshaw, R., Jackson, L. C., Dubois, C., Iovino, D., Zuo, H., Perez, R. C., Dong, S., Kersalé, M., Mayer, M., Mayer, J., Speich, S., and Lamont, T.: Overturning and heat transport variations in the South Atlantic in an ocean reanalysis ensemble, State Planet, 1-osr7, 4 pp., https://doi.org/10.5194/sp-1-osr7-4-2023, 2022. a
Bell, B., Hersbach, H., Simmons, A., Berrisford, P., Dahlgren, P., Horányi, A., Muñoz-Sabater, J., Nicolas, J., Radu, R., Schepers, D., Soci, C., Villaume, S., Bidlot, J.-R., Haimberger, L., Woollen, J., Buontempo, C., and Thépaut, J.-N.: The ERA5 global reanalysis: Preliminary extension to 1950, Q. J. Roy. Meteor. Soc., 147, 4186–4227, https://doi.org/10.1002/qj.4174, 2021. a
Bengtsson, L., Hagemann, S., and Hodges, K. I.: Can climate trends be calculated from reanalysis data?, J. Geophys. Res.-Atmos., 109, D11111, https://doi.org/10.1029/2004JD004536, 2004. a
Boers, N.: Observation-based early-warning signals for a collapse of the Atlantic Meridional Overturning Circulation, Nat. Clim. Change, 11, 680–688, https://doi.org/10.1038/s41558-021-01097-4, 2021. a
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Short summary
This study investigates the temporal stability and reliability of winter-month trends of air–sea heat fluxes from ERA5 forecasts over the North Atlantic basin for the period 1950–2019. Driving forces of trends and the impact of modes of climate variability and analysis increments on air–sea heat fluxes are investigated. Finally, a new and independent estimate of the Atlantic Meridional Overturning Circulation weakening is provided and associated with a decrease in air–sea heat fluxes.
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