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For potential wind power sites where the Weibull model of the wind speed distribu- tion is applicable ended use of the Rayleigh distribution for commercially exploitable wind power sites with Experience to date suggests that the Weibull.
We develop and analyze a methodology to partition the received signal-to-noise ratio SNR into a finite number of states according to the time duration of each state. Each state corresponds to a different channel quality indicated by the bit-error rate BER. The number of states and SNR partitions are determined by the fading speed of the channel.
Computer simulations are performed to verify the accuracy of the model. Article :. Date of Publication: Nov
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suggested that for a slowly evaporating sessile droplet containing a macromolecular solution, a quite-fast fluid flow could be generated making use of the.
The Rayleigh scatter at high temperatures was correlated to the formation and modification of nanogratings in the fiber core. Information gathered by these fiber sensor tools can be used to verify simulation results or operated in a process-control system to improve the operational efficiency and longevity of SOFC-based energy generation systems. Solid oxide fuel cell SOFC technology is a promising and versatile energy generation scheme.
On the Rayleigh Wave Speed in Orthotropic Elastic Solids
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Rayleigh scattering is usually considered to be the elastic scattering of photons from subwavelength physical objects, such as small particles or.
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Community events in Rayleigh, United Kingdom
Rayleigh waves are a type of surface acoustic wave that travel along the surface of solids. They can be produced in materials in many ways, such as by a localized impact or by piezo-electric transduction , and are frequently used in non-destructive testing for detecting defects. Rayleigh waves are part of the seismic waves that are produced on the Earth by earthquakes. When guided in layers they are referred to as Lamb waves , Rayleigh—Lamb waves, or generalized Rayleigh waves. Rayleigh waves are a type of surface wave that travel near the surface of solids.
Rayleigh waves include both longitudinal and transverse motions that decrease exponentially in amplitude as distance from the surface increases.
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The dense AlpArray network allows studying seismic wave propagation with high spatial resolution. Here we introduce an array approach to measure arrival angles of teleseismic Rayleigh waves. The approach combines the advantages of phase correlation as in the two-station method with array beamforming to obtain the phase-velocity vector. The cause of these intriguing spatial patterns is discussed.
A simple wave-propagation modelling example using an isolated anomaly and a Gaussian beam solution suggests that much of the complexity can be explained as a result of wave interference after passing a structural anomaly along the wave paths. This indicates that arrival-angle information constitutes useful additional information on the Earth structure, beyond what is currently used in inversions.