dc.description.abstract | While wind driven waves affect erosion, sediment resuspension, and flow in shallow
estuaries like the Indian River Lagoon (IRL), neither winds nor waves are well observed in
this environment. In order to calculate accurate significant wave heights, the winds used
for the calculation must be consistent with the observed winds over the lagoon. Given the
complex land/water geometry and subsequent limited fetch, a probabilistic approach is
used to produce a representative wind field over the IRL. Observed winds, near the IRL,
are used to sample wind distributions obtained from 180 high resolution atmospheric
model simulations in order to generate a synthetic wind time series. Significant wave
heights are then calculated using a well-known wave height parameterization, modified for
shallow water, which depends on the synthetic winds, fetch, and bottom topography.
Results within the IRL indicate that significant wave heights appear to be sensitive to wind
direction in addition to wind speed. The bathymetry also has an impact on significant wave
heights in the shallow estuary. Due to the lack of observations, the parameterized
significant wave heights are compared to wave model simulations. Statistics indicate that
the parameterized wave heights are biased low compared to the model. However these
differences can, in part, be explained by a mismatch between the model and
parameterization topography. The wave parameterization is a less expensive alternative to
running probabilistic, long term, hydrodynamic-wave model simulations within shallow
water estuaries such as the IRL. | en_US |