1993
DOI: 10.1016/0377-0265(93)90049-d
|View full text |Cite
|
Sign up to set email alerts
|

Blocking and trapping of waves in an inhomogeneous flow

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
8
0
1

Year Published

1996
1996
2016
2016

Publication Types

Select...
7
1

Relationship

2
6

Authors

Journals

citations
Cited by 21 publications
(9 citation statements)
references
References 12 publications
0
8
0
1
Order By: Relevance
“…There are other variations of the Fourier-based methods, such as the spectrogram (see, for example, Oppenheim & Schafer 1989); wavelet analysis for time series (see, for example, Chan 1995, Farge 1992, and Long et al 1993a, and two-dimensional images (Spedding et al 1993); the Wigner-Ville distribution (see, for example, Claasen &Mecklenbräuker 1980 andCohen 1995); the evolutionary spectrum (see, for example, Priestley 1965); the empirical orthogonal function expansion, also known as the principal component analysis, or singular value decomposition method; and some miscellaneous methods such as least square estimation of the trend, smoothing by moving averaging, and differencing to generate stationary data. All the above methods are designed to modify the global representation of the Fourier analysis, but they all failed in one way or the other, as discussed by Huang et al (1998a) and demonstrated here.…”
Section: Discussionmentioning
confidence: 99%
“…There are other variations of the Fourier-based methods, such as the spectrogram (see, for example, Oppenheim & Schafer 1989); wavelet analysis for time series (see, for example, Chan 1995, Farge 1992, and Long et al 1993a, and two-dimensional images (Spedding et al 1993); the Wigner-Ville distribution (see, for example, Claasen &Mecklenbräuker 1980 andCohen 1995); the evolutionary spectrum (see, for example, Priestley 1965); the empirical orthogonal function expansion, also known as the principal component analysis, or singular value decomposition method; and some miscellaneous methods such as least square estimation of the trend, smoothing by moving averaging, and differencing to generate stationary data. All the above methods are designed to modify the global representation of the Fourier analysis, but they all failed in one way or the other, as discussed by Huang et al (1998a) and demonstrated here.…”
Section: Discussionmentioning
confidence: 99%
“…A review of wavelet in geosciences can be found in FoufoulaGeorgiou and Kumar (1995). This paper will concentrate on the most recent contributions in the field of earth sciences: † Fluid mechanics with isolation of coherent structures in turbulent flows (Argoul et al, 1989;Liandrat et al, 1990;Farge and Rabreau, 1988;Farge, 1992;Long et al, 1993;Higuchi et al, 1994;Katul et al, 1994Katul et al, , 1995aKatul et al, , 1995b. † Meteorology with temporal variability of coherent convective storm structures (Kumar and Foufoula-Georgiou, 1993;Takeuchi et al, 1994;Venugopal and Foufoula-Georgiou, 1996;Kumar, 1996), and examination of turbulence structures above forest canopy (Turner et al, 1994;Katul and Parlange, 1995a,b;Szilagi et al, 1999;Katul et al, 1998Katul et al, , 2001.…”
Section: The Wavelet Transform In Geosciencesmentioning
confidence: 98%
“…The well known Fourier spectral analysis works well for strictly periodic or stationary random functions of time. To deal with nonperiodic or nonstationary functions, a number of methods have been introduced, such as the Spectrogram (10), the Wavelet analysis (11)(12)(13)(14), the Wigner-Ville distribution (15,16), the Evolutionary Spectrum (17), the Modal Analysis (18), and some others, all designed to modify the global representation of the Fourier analysis. They all failed in one way or another as discussed by Huang et al (19,20).…”
Section: Materials and Experimental Methodsmentioning
confidence: 99%