  We study deep water ocean wind-driven waves in strait, with wind directed
orthogonally to the shore, through exact Hasselmann equation. Despite of
"dissipative" shores - we do not include any reflection from the coast lines -
we show that the wave turbulence evolution can be split in time into two
different regimes. During the first wave propagate along the wind, and the
wind-driven sea can be described by the self-similar solution of the Hasselmann
equation like in the open sea. The second regime starts later in time, after
significant enough wave energy accumulation at the down-wind boundary. Since
this moment the ensemble of waves propagating against the wind starts its
formation. Also, the waves, propagation along the strait start to appear. The
wave system eventually reaches asymptotic stationary state in time, consisting
of two co-existing states: the first, self-similar wave ensemble, propagating
with the wind, and the second, quasi-monochromatic waves, propagating almost
orthogonal to the wind direction and tending to slant against the wind at the
angle of 15 degrees closer to the wave turbulence origination shore line. These
"secondary waves" appear only due to intensive nonlinear wave interaction. The
total wave energy exceeds its "expected value" approximately by the factor of
two, with respect to estimated in the absence of the shores. It is expected
that in the reflective shores presence this amplification will grow
essentially. We propose to call this laser-like Nonlinear Ocean Waves
Amplification mechanism by the acronym NOWA.
