In this contribution the wind jet dynamics in the northern margin of the
Ebro River shelf (NW Mediterranean Sea) are investigated using coupled
numerical models. The study area is characterised by persistent and
energetic offshore winds during autumn and winter. During these seasons, a
seaward wind jet usually develops in a ∼ 50 km wide band
offshore. The COAWST (Coupled Ocean–Atmosphere–Wave–Sediment Transport) modelling system was implemented in the region with a set of
downscaling meshes to obtain high-resolution meteo-oceanographic outputs.
Wind, waves and water currents were compared with in situ observations and
remote-sensing-derived products with an acceptable level of agreement.
Focused on an intense offshore wind event, the modelled wind jet appears in
a limited area offshore with strong spatial variability. The wave pattern
during the wind jet is characterised by the development of bimodal
directional spectra, and the ocean circulation tends to present well-defined
two-layer flow in the shallower region (i.e. inner shelf). The outer shelf
tends to be dominated by mesoscale dynamics such as the slope current. Due
to the limited fetch length, ocean surface roughness considering sea state
(wave–atmosphere coupling) modifies to a small extent the wind and
significant wave height under severe cross-shelf wind events. However, the
coupling effect in the wind resource assessment may be relevant due to the
cubic relation between the wind intensity and power
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