Sentence examples for most energetic waves from inspiring English sources

The sources of the most energetic waves are narrowly and stably localized into two closely adjacent azimuthal windows with mutually different wave spectral characteristics.

The most energetic waves incoming from the SE direction are poorly accompanied by reflections from the nearest coast, where wave scattering, wave-wave conversion, and dissipation may be significant.

Global wave energy inventories show that the West Coast of Canada possesses one of the most energetic wave climates in the world, with an annual wave energy flux of 40 50 kW/m at the continental shelf.

The most commonly occurring wave state has significant wave height in the interval 0.15 0.25m and energy period in the interval 5.05 5.15s while the most energetic wave state occurs for significant wave height in the interval of 0.75 0.85m and energy period in the interval 5.25 and 5.30s.

The most commonly occurring wave state has significant wave height in the interval 0.25 0.45 m and energy period in the interval 11.2 12.2s while the most energetic wave state occurs for significant wave height in the interval of 0.58 and 0.75m and energy period in the interval 11.8 and 12.8s.

Application of a slant-stacking technique revealed that the most energetic IG waves are incoming across the Nankai Trough from the Philippine Sea with limited energy of reflected waves back from the nearest coast.

Figure 6a shows the daily variations of the incoming direction of the most energetic IG waves throughout the 3 years, where the color indicates the PSD value.

During mean conditions, the most energetic ocean waves are observed during the DJF season for both ENSO phases (El Niño and La Niña) for most of the Caribbean Sea.

These observations suggest that the amplified IG waves from the NE to ENE direction were generated secondarily at far distances from the primary (typhoon) source.We measured the incoming direction of the most energetic IG waves during the 3-year period.

Stacking was accomplished by using a slowness vector that makes the stacked IG wave most energetic.

It was ensured that the selected years for which the WTR was deployed contained no data recorded in cyclonic weather conditions, which would inevitably lead to biased results when it comes to selecting the most energetic region for tapping in surface wave energy.