Description Usage Arguments Value Note Author(s) References Examples
Determine significance of wavelet coherence
1 2 3 |
nrands |
number of Monte Carlo randomizations. Default is 300. |
lag1 |
vector containing the AR(1) coefficient of each time series. |
dt |
length of a time step. |
ntimesteps |
number of time steps in time series. |
pad |
pad the values will with zeros to increase the speed of the transform. Default is |
dj |
spacing between successive scales. Default is 1/12. |
s0 |
smallest scale of the wavelet. Default is |
J1 |
number of scales - 1. |
max.scale |
maximum scale |
mother |
type of mother wavelet function to use. Can be set to |
sig.level |
significance level to compute. Default is |
quiet |
Do not display progress bar. Default is |
Returns significance matrix containing the sig.level
percentile of wavelet
coherence at each time step and scale.
The Monte Carlo randomizations can be extremely slow for large datasets. For instance, 1000 randomizations of a dataset consisting of 1000 samples will take ~30 minutes on a 2.66 GHz dual-core Xeon processor.
Tarik C. Gouhier (tarik.gouhier@gmail.com)
Code based on WTC MATLAB package written by Aslak Grinsted.
Cazelles, B., M. Chavez, D. Berteaux, F. Menard, J. O. Vik, S. Jenouvrier, and N. C. Stenseth. 2008. Wavelet analysis of ecological time series. Oecologia 156:287-304.
Grinsted, A., J. C. Moore, and S. Jevrejeva. 2004. Application of the cross wavelet transform and wavelet coherence to geophysical time series. Nonlinear Processes in Geophysics 11:561-566.
Torrence, C., and G. P. Compo. 1998. A Practical Guide to Wavelet Analysis. Bulletin of the American Meteorological Society 79:61-78.
Torrence, C., and P. J. Webster. 1998. The annual cycle of persistence in the El Nino/Southern Oscillation. Quarterly Journal of the Royal Meteorological Society 124:1985-2004.
1 2 | ## Not run: wtcsig=wtc.sig(nrands, lag1 = c(d1.ar1, d2.ar1), dt,
## pad, dj, J1, s0, mother = morlet)
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biwavelet 0.20.17 loaded.
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