Wavelength and wavenumber are two very important concepts discussed in physics and various other fields. Wavelength is the distance between two consecutive points which are in the same phase. Wavenumber is the number of wavelengths in a given distance along the propagation of the wave. In this art...
Twitter Google Share on Facebook probability wave Wikipedia n. A wave whose amplitude at a given region and over a given time interval corresponds to the probability of observing a given particle within that region in that time. American Heritage® Dictionary of the English Language, Fifth Editi...
Arctic sea ice thickness changes in terms of sea ice age[J]. Acta Oceanologica Sinica, 2016, 35(10): 1-10. doi: 10.1007/s13131-016-0922-x [7] LI Tao, ZHAO Jinping. An impact assessment of sea ice on ocean optics observations in the marginal ice zone of the Arctic[J]. Acta ...
where one uses only linear logical terms of the expansion, and changes to the inverse by simply swapping the base and the power. It is useful to re-express this result in the language of a quantum system defined in an infinite spatial volume, where the corresponding Hilbert space is divided...
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Our choice of discussing different components of the S vector in terms of SH and SV clearly has little significance for whole-space solutions; it merely sets the stage for subsequent discussions in the Earth coordinate system. Clearly, the total S-wave motion is a vector displacement in the ...
The droplet is able to read its memory (the two last terms in Eq. (1)) and to edit its memory (through the Bessel function in Eq. (2)), similarly to a Turing machine55. Erasing the memory is also possible with a specific protocol55. The concept of memory is therefore justified ...
The other symbols are the same as those Equation (1-71): Sh is the power spectral density function of the ladder histogram. Connect each endpoint of the ladder in the ladder histogram into a continuous curve as shown in Figure 1-15, and we get the continuous spectrum diagram. If the ...
On a sphere, it is convenient to expand lateral heterogeneity in terms of surface spherical harmonics Ylm(θ, ϕ) as function of geographic coordinates θ and ϕ, so that δc/c0 is [21]δc(ω)c0(ω)=∑i=0LM∑m=−llclm(ω)Ylm(θ,φ) where the clm are complex coefficients and...
The amplitudes of high-frequency seismic waves generated by local and/or regional earthquakes vary from site to site, even at similar hypocentral distances. It had been suggested that, in addition to local site effects (e.g., variable attenuation and amplification in surficial layers), complex ...