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The results indicated that in the coastal area of Lithuania, waves approaching from western directions prevail with mean wave height of 0.9 m.
In the Baltic Sea Lithuanian nearshore, the mean wave height ranges from 0.68 to 0.98 m, while the estimated mean energy flux reaches from 0.69 to 1.90 kW m−1 during a year of different wave intensity.
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The results show that the mean wave heights decrease from south to north and from sea to land in general.
The mean wave heights in the winter season have the highest values, mainly due to the effect of winter monsoon winds.
For each monitoring site, mean wave heights were recorded with respect to their angle of exposure, using the wave-rose data.
Weather was an important factor during the survey period of 4 15 January 2006, as mean wave heights of 3 m–4.5 m were recorded on several days.
Tidal range is mesotidal (2.0 m) and the mean significant wave height is 0.6 m with an average period of 3.6 s.
The erosional trend peaked in 1995 at a time during which the values for monthly winter mean significant wave height were notably high.
Using previously calibrated ("default") values of a free parameter γ, all models predict the observations reasonably well (median root-mean-square wave height errors are between 10%and20%0%) at all field sites.
Equations are also given for mean flow thickness, RMS wave height, mean velocity, and velocity of the wave front down the landward-side slope.
New equations were developed to estimate distribution of instantaneous discharge, distribution of individual wave volumes as well as flow parameters on landward-side slope, including mean flow thickness, RMS wave height, mean velocity, and wave front velocity for the RCC strengthened levee.
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CEO of Professional Science Editing for Scientists @ prosciediting.com