Dominance of the mean sea level in the high-percentile sea levels time evolution with respect to large-scale climate variability: a Bayesian statistical approach

• Published in: Environmental Research Letters
• Main Authors: Rohmer, Jeremy, Le Cozannet, Gonéri
• Other Authors: Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2019
• Subjects: climate indices; NORTH-ATLANTIC; OSCILLATION; Kalman-filter; mean sea level; extremes; Bayesian structure time series model; EXTENSION; [SDU.STU.AG]Sciences of the Universe [physics]/Earth Sciences/Applied geology; Canada; North Atlantic; North Atlantic oscillation
• Online Access: https://hal.archives-ouvertes.fr/hal-02380692; https://hal.archives-ouvertes.fr/hal-02380692/document; https://hal.archives-ouvertes.fr/hal-02380692/file/hal-02380692.pdf; https://doi.org/10.1088/1748-9326/aaf0cd

International audience Changes in mean sea level (MSL) are a major, but not the unique, cause of changes in high-percentile sea levels (HSL), e.g. the annual 99.9th quantile of sea level (among other factors, climate variability may also have huge influence). To unravel the respective influence of each contributor, we propose to use structural time series models considering six major climate indices (CI) (Artic Oscillation, North Atlantic Oscillation, Atlantic Multidecadal Oscillation, Southern Oscillation Index, Nino 1 + 2 and Nino 3.4) as well as a reconstruction of MSL. The method is applied to eight century-long tide gauges across the world (Brest (France), Newlyn (UK), Cuxhaven (Germany), Stockholm (Sweden), Gedser (Danemark), Halifax (Canada), San Francisco (US), and Honolulu (US)). The treatment within a Bayesian setting enables to derive an importance indicator, which measures how often the considered driver is included in the model. The application to the eight tide gauges outlines that MSL signal is a strong driver (except for Gedser), but is not unique. In particular, the influence of Artic Oscillation index at Cuxhaven, Stockholm and Halifax, and of Nino Sea Surface Temperature index 1 + 2 at San Francisco appear to be very strong as well. Asimilar analysis was conducted by restricting the time period of interest to the 1st part of the 20th century. Over this period, we show that the MSL dominance is lower, whereas an ensemble of CI contribute to a large part to HSL time evolution as well. The proposed setting is flexible and could be applied to incorporate any alternative predictive time series such as river discharge, tidal constituents or vertical ground motions where relevant.