Abstract. This research examines the nonstationary dynamics of extreme surges along
the English Channel coasts and seeks to make their connection to the climate
patterns at different timescales by the use of a detailed spectral analysis
in order to gain insights into the physical mechanisms relating the global
atmospheric circulation to the local-scale variability of the monthly
extreme surges. This variability highlights different oscillatory components
from the interannual (∼1.5, ∼2–4,
∼5–8 years) to the interdecadal (∼12–16 years) scales with mean explained variances of ∼25 %–32 % and ∼2 %–4 % of the total variability, respectively.
Using the two hypotheses that the physical mechanisms of the atmospheric
circulation change according to the timescales and their connection with the
local variability improves the prediction of the extremes, we have
demonstrated statistically significant relationships of ∼1.5, ∼2–4, ∼5–8 and
12–16 years with the different climate oscillations of sea level pressure,
zonal wind, North Atlantic Oscillation and Atlantic Multidecadal
Oscillation, respectively. Such physical links have been used to implement the parameters of the
time-dependent generalized extreme value (GEV) distribution models. The introduced climate information
in the GEV parameters has considerably improved the prediction of the
different timescales of surges with an explained variance higher than
60 %. This improvement exhibits their non-linear relationship with the
large-scale atmospheric circulation.