EGU23-8186
https://doi.org/10.5194/egusphere-egu23-8186
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Changes in extreme sea levels along the North Atlantic coasts, over the last century

Lucia Pineau-Guillou1, Pascal Lazure1, Guy Wöppelmann2, Jean-Baptiste Roustan3, and Markus Reinert4
Lucia Pineau-Guillou et al.
  • 1Ifremer, Laboratory for Ocean Physics and Satellite remote sensing (LOPS), Brest, France (lucia.pineau.guillou@ifremer.fr)
  • 2LIENNS, University of La Rochelle-CNRS, La Rochelle, France
  • 3UBO, Laboratory for Ocean Physics and Satellite remote sensing (LOPS), Brest, France
  • 4Leibniz Institute for Baltic Sea Research Warnemünde, Rostock, Germany

Extreme sea levels are the joint contribution of mean sea level, tide and storm surges. The ClimEx project investigates changes in tide and storm surges over the last century, along the North Atlantic coasts. Concerning the tide, we investigated the long-term changes of the principal tidal component M2, from 1846 to 2018 (Pineau-Guillou et al., 2021). The M2 variations are consistent at all the stations in the North-East Atlantic. The changes started long before the 20th century and are not linear. Regarding the possible causes of the observed changes, the similarity between the North Atlantic Oscillation and M2 variations in the North-East Atlantic suggests a possible influence of the large-scale atmospheric circulation on the tide. A possible underlying mechanism is discussed. Concerning the storm surges, we found a clear shift in the storm surge season at Brest (France), between 1950 and 2000 (Reinert et al., 2021). Extreme storm surge events occurred three weeks earlier (mid-December instead of beginning of January) in the winter 2000 than in the 1950s. Analysis of additional stations in Europe reveals a large-scale process (Roustan et al., 2022). Temporal shifts are positive (later events) in northern Europe, and negative (earlier events) in southern Europe. Such a tendency is similar to the one already reported for European river floods between 1960 and 2010 (Blöschl et al., 2017).

 

References

[1] Pineau-Guillou L., Lazure P. and Wöppelmann G. (2021). Large-scale changes of the semidiurnal tide along North Atlantic coasts from 1846 to 2018. Ocean Sci., 17, 17–34. https://doi.org/10.5194/os-17-17-2021

[2] Reinert M., Pineau-Guillou L., Raillard N., Chapron B. (2021). Seasonal shift in storm surges at Brest revealed by extreme value analysis. J. Geophys. Res. Oceans, 126, e2021JC017794. https://doi.org/10.1029/2021JC017794

[3] Roustan J.-B., Pineau-Guillou L., Chapron B., Raillard N., Reinert M. (2022). Shift of the storm surge season in Europe due to climate variability. Sci. Rep., 12, 8210. https://doi.org/10.1038/s41598-022-12356-5

[4] Blöschl G., Hall J., Parajka J., Perdigão R. A. P., Merz B., Arheimer B. et al. (2017). Changing climate shifts timing of European floods. Science, 357(6351), 588–590. https://doi.org/10.1126/science.aan2506

How to cite: Pineau-Guillou, L., Lazure, P., Wöppelmann, G., Roustan, J.-B., and Reinert, M.: Changes in extreme sea levels along the North Atlantic coasts, over the last century, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-8186, https://doi.org/10.5194/egusphere-egu23-8186, 2023.