Teleconnections and Extreme Ocean States in the Northeast Atlantic Ocean
The Northeast Atlantic possesses an energetic and variable wind and wave
climate which has a large potential for renewable energy extraction; for
example along the western seaboards off Ireland. The role of surface winds in
the generation of ocean waves means that global atmospheric circulation
patterns and wave climate characteristics are inherently connected. In
quantifying how the wave and wind climate of this region may change towards
the end of the century due to climate change, it is useful to investigate the
influence of large scale atmospheric oscillations using indices such as the
North Atlantic Oscillation (NAO), the East Atlantic pattern (EA) and the
Scandinavian pattern (SCAND). In this study a statistical analysis of these
teleconnections was carried out using an ensemble of EC-Earth global climate
simulations run under the RCP4.5 and RCP8.5 forcing scenarios, where EC-Earth
is a European-developed atmosphere ocean sea-ice coupled climate model. In
addition, EC-Earth model fields were used to drive the WAVEWATCH III wave
model over the North Atlantic basin to create the highest resolution wave
projection dataset currently available for Ireland. Using this dataset we
analysed the correlations between teleconnections and significant wave
heights (Hs) with a particular focus on extreme ocean states using a range
of statistical methods. The strongest, statistically significant correlations
exist between the 95th percentile of significant wave height and the NAO.
Correlations between extreme Hs and the EA and SCAND are weaker and not
statistically significant over parts of the North Atlantic. When the NAO is
in its positive phase (NAO+) and the EA and SCAND are in a negative phase
(EA−, SCAND−) the strongest effects are seen on 20-year return levels of
extreme ocean waves. Under RCP8.5 there are large areas around Ireland where
the 20-year return level of Hs increases by the end of the century,
despite an overall decreasing trend in mean wind speeds and hence mean Hs.
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