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Both the average wave direction over the entire frequency range (0.03 0.58 Hz) and the direction corresponding to the peak frequency are used in practice.
Analyses are presented relating to: (i) the relative wave height (H/d); (ii) the wave celerity; (iii) the two-dimensional distribution of the particle velocities components; finally (iv) the average wave direction and spreading angle were carried out.
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Average difference between the mean wave direction at peak frequency and the average over the frequency related to spectral energy more than 20% of maximum value is less, around 13°. Study shows that average difference in the sea and swell directions is around 39°.
Santolík et al. (2003) showed Cluster observation that chorus propagate nearly parallel to the field lines in the region close to the magnetic equator and the average wave vector directions gradually become inclined at higher latitudes (approximately 10°).
This is because most of dominant incoming waves were the direct wave ( direction) from the TX to the RX, the reflected wave (+ direction) from the wall behind the TX, and the reflected wave ( direction) from the wall behind the RX.
Fig. 7b shows the incoming wave direction at Roches Noires for the month of April, averaged over 3-years period (2012 2014).
There are two different approaches to determine wave direction.
The analysis is carried out starting from significant wave height and wave direction time series.
The predominant wave direction is easterly.
Indeed, Machemer showed that membrane voltage affects the metachronal wave direction in Paramecium (Machemer, 1972).
At present, such radars are already used to detect averaged characteristics of waves, such as the peak period, significant wave height, wave directions and currents.
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