emd {EMD} | R Documentation |
Empirical Mode Decomposition
Description
This function performs empirical mode decomposition.
Usage
emd(xt, tt=NULL, tol=sd(xt)*0.1^2, max.sift=20, stoprule="type1",
boundary="periodic", sm="none", smlevels=c(1), spar=NULL, alpha=NULL,
check=FALSE, max.imf=10, plot.imf=FALSE, interm=NULL, weight=NULL)
Arguments
xt |
observation or signal observed at time |
tt |
observation index or time index |
tol |
tolerance for stopping rule of sifting. If |
max.sift |
the maximum number of sifting |
stoprule |
stopping rule of sifting. The |
boundary |
specifies boundary condition from “none", “wave", “symmetric", “periodic" or “evenodd". See Zeng and He (2004) for |
sm |
specifies whether envelop is constructed by interpolation, spline smoothing, kernel smoothing, or local polynomial smoothing. Use “none" for interpolation, “spline" for spline smoothing, “kernel" for kernel smoothing, or “locfit" for local polynomial smoothing. See Kim et al. (2012) for detalis. |
smlevels |
specifies which level of the IMF is obtained by smoothing other than interpolation. |
spar |
specifies user-supplied smoothing parameter of spline smoothing, kernel smoothing, or local polynomial smoothing. |
alpha |
deprecated. |
check |
specifies whether the sifting process is displayed. If |
max.imf |
the maximum number of IMF's |
plot.imf |
specifies whether each IMF is displayed. If |
interm |
specifies vector of periods to be excluded from the IMF's to cope with mode mixing. |
weight |
deprecated. |
Details
This function performs empirical mode decomposition.
Value
imf |
IMF's |
residue |
residue signal after extracting IMF's from observations |
nimf |
the number of IMF's |
References
Huang, N. E., Shen, Z., Long, S. R., Wu, M. L. Shih, H. H., Zheng, Q., Yen, N. C., Tung, C. C. and Liu, H. H. (1998) The empirical mode decomposition and Hilbert spectrum for nonlinear and nonstationary time series analysis. Proceedings of the Royal Society London A, 454, 903–995.
Huang, N. E. and Wu, Z. (2008) A review on Hilbert-Huang Transform: Method and its applications to geophysical studies. Reviews of Geophysics, 46, RG2006.
Kim, D., Kim, K.-O. and Oh, H.-S. (2012) Extending the Scope of Empirical Mode Decomposition using Smoothing. EURASIP Journal on Advances in Signal Processing, 2012:168, doi: 10.1186/1687-6180-2012-168.
Zeng, K and He, M.-X. (2004) A simple boundary process technique for empirical mode decomposition. Proceedings of 2004 IEEE International Geoscience and Remote Sensing Symposium, 6, 4258–4261.
See Also
Examples
### Empirical Mode Decomposition
ndata <- 3000
tt2 <- seq(0, 9, length=ndata)
xt2 <- sin(pi * tt2) + sin(2* pi * tt2) + sin(6 * pi * tt2) + 0.5 * tt2
try <- emd(xt2, tt2, boundary="wave")
### Ploting the IMF's
par(mfrow=c(try$nimf+1, 1), mar=c(2,1,2,1))
rangeimf <- range(try$imf)
for(i in 1:try$nimf) {
plot(tt2, try$imf[,i], type="l", xlab="", ylab="", ylim=rangeimf,
main=paste(i, "-th IMF", sep="")); abline(h=0)
}
plot(tt2, try$residue, xlab="", ylab="", main="residue", type="l", axes=FALSE); box()