Sentence examples for origin of the wave from inspiring English sources

An important degree of uncertainty regards the methodology aiming to the definition of the origin of the wave responsible for their deposition.

In order to identify the origin of the wave energy reduction and to properly assess the wave damping performance of the mangrove forest, a classification of the wave evolution modes is introduced for waves propagating in the 2 m- and 1 m-wide flumes (i.e. with and without the forest model, respectively).

In this paper, which focuses on instrumental technique, we do not undertake detailed analysis of origin of the observed event, but do note below that an association with field-line resonance is not likely, nor is an origin of the wave power on the flank.

However, the experimental studies utilizing the same type of electrodes show that actual origin of the wave can be 1 to 2 millimeters away from the stimulating lead location [ 26].

Though the mathematical treatment is detailed, the underlying origin of the waves can be understood qualitatively: changing magnetic fields produce electric fields, and changing electric fields produce magnetic fields.

The origin of the waves appears to be due to substorm/stormrelated instabilities and, in the dayside, to solar wind compressions of the magnetopause.

The origins of the wave groups are estimated to be on the deeper side of the hypocenter, and the origins are located close to each other (Kurahashi and Irikura, 2011; Asano and Iwata, 2012).

If the origin of the second wave group is the arrival of the rupture at the free surface, the second wave group would appear in the result for case 2. Fig. 11.

In addition to delineating the spectrum of tidal components at 110 km as a second objective of this study, we seek to explain the origins of the waves and the nature of their seasonal-latitudinal structures.

The spectra in Figures 3, 4, and 5 provide a broad overview of the tidal components that are present and begin to provide some insight into possible origins of the waves.

In addition, Table 2 contains a compilation of the likely origins of the waves (lower atmosphere heating and nonlinear wave-wave interactions) and the predominant Hough mode composition of the most well-defined seasonal-latitudinal structures at 110 km. Figure 11 Latitude vs. month depictions of multi-year average SABER temperature amplitudes.