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I was checking out the mathworks site for the new version of the CWT function http://www.mathworks.com/help/wavelet/ref/cwt.html and realised that cwt no longer supports user selectable wavelets such as cmorx.x, dbx, dmey etc. You only have three options : morse', 'amor', and 'bump'

Moreover you no longer can obtain the CWT of a signal at a specified scale, or, for that matter, at user selectable scales likewise c=cwt(signal,'scales,wavelet_type)

Strangely enough in the r2016b WaveletAnalyzer(ex wavemenu) the wavelet selection includes all the previous wavelets (cmorx.x, dbx, dmey, gaussx, haar). Moreover the user can select the scale, likewise in the old cwt.

Does that mean that there is no command line cwt command that apply these wavelets, and user scale selection???

Walter Roberson
on 11 Oct 2016

The R2016b release notes say

Continuous Wavelet Transform: Analyze signals with improved automatic selection of wavelet and scales

This release provides an updated version of the continuous wavelet transform, cwt, and a new inverse transform, icwt, for reconstructing the original signal. These functions are easier to use because they have simple interfaces and include default values for the wavelet and scales and frequency and period ranges are easy to specify. When you use the updated cwt, which use analytic wavelets and L1 normalization, icwt produce a more accurate reconstruction.

Compatibility Considerations

The old version of cwt continues to work, however, updating existing code to use the new version of cwt is recommended. Both the old and updated versions use the same function name. The inputs to the function determine automatically which version is used.

====

The documentation page for cwt says you can also look at https://www.mathworks.com/help/wavelet/ref/cwtold.html

Walter Roberson
on 12 Oct 2016

Walter Roberson
on 13 Oct 2016

I recommend you open a support case telling Mathworks that you need the old functionality and telling them they need to continue to support it. You can visit https://www.mathworks.com/support/servicerequests/index.html and open a support case from there. Mathworks support does not follow this Answers facility.

(I do not work for Mathworks, and I do not use this facility.)

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Wayne King
on 13 Oct 2016

Edited: Wayne King
on 13 Oct 2016

Paramonte, I posted this response on another thread where you posted a comment. I will repeat the essential content here. As I said in the other post, I would be very interested in engaging with you so please do contact me.

There was already CWTFT in the toolbox for a number of releases that used an FFT-based algorithm (that DFT-based approach to the CWT long preceded Torrence and Compo by the way). The new CWT algorithm features Morse wavelets, which have parameters that can be adjusted to give a very large family of analytic wavelets. In fact, most analytic wavelets in use are just special cases of Morse wavelets as was proved by Lilly and Olhede. We have received a lot of feedback from customers that they are confused by having to specify scales and in fact they quite often get the scale concept wrong and use scales that don't allow them to actually find the phenomena they are looking for. The old CWT had absolutely no defaults. The user had the burden of specifying everything. As I mentioned for many non-experts, having to pick a wavelet was daunting, never mind having to construct a meaningful scale vector. Scale for the wavelet transform should be logarithmically spaced for example and the scales should take into account the support of the wavelet. Neither of those things were built into the old CWT.

For time-frequency (time-scale) analysis which is a major use case for continuous wavelet analysis, many of the orthogonal or biorthogonal wavelets which are quite useful for discrete analysis are inappropriate and lead in many instances to people obtaining a misleading analysis of their data. Orthogonal and biorthogonal wavelets are designed for dyadic scales, which are much more widely spaced that the typical scales in continuous wavelet analysis.

Having said all that, if you want to use the old CWT, that interface still works. In fact, the new CWT parses the input and determines if you are using the old syntax. If so, it will give you the older algorithm. I would sincerely welcome the opportunity to discuss these things further. Feel free to contact me through my profile. I will respond. I would very much be interested in any specific use cases where the old CWT allows one to obtain some insight not obtainable with the new CWT. I am always very interested in getting feedback from users on how to make things better.

We never "not recommend" something lightly. That is not to say that somehow we are infallible, but a lot of thought and customer feedback goes into those decisions.

Hope that helps, Wayne

Paul C
on 9 Jul 2017

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Wayne King
on 13 Oct 2016

Dear Paramonte, with respect to naming this is always a hard decision. The acronym CWT is well established so users look for it. Users also expressed some confusion at why we had CWT and CWTFT, and which one should they use. The new CWT algorithm also lends itself to an inverse algorithm which the old one did not, so now we have CWT and ICWT for the inverse. The ICWT accepts a frequency or period band input so you can do a frequency-localized reconstruction.

As I suggested, we specifically implemented the new CWT in a way that you can simply call the old one if you wish.

I would welcome a detailed discussion with you as I offered. But we have seen many users struggle with scale and specifying scales. For example, users will specify scales without taking into account the support of the analyzing wavelet. As a result they would have many scales where the wavelet extended well beyond the extent of their data. So in fact, they had no wavelet at all (there was not even one oscillation in the extent of the data). Or they would similarly use scales which were too small and therefore did not provide any wavelet analysis.

Also, as you are no doubt aware, the scale-to-frequency conversion is not equally good for all wavelets. For the Morse wavelets and the default we use, it is quite good because that wavelet is symmetric and well-localized in the Fourier domain. That is also true of the 'bump' wavelet and 'amor' (Morlet) wavelets supported by the new CWT.

For example, here is the default Morse wavelet in the Fourier domain with a vertical line at its predicted center frequency

omega = 0:0.001:(2*pi);

psihat = omega.^20.*0.0051.*exp(-omega.^3);

plot(omega,psihat); grid on; hold on;

title('Default Morse Wavelet -- Fourier Domain');

plot([(20/3)^(1/3) (20/3)^(1/3)],[0 2.5],'k')

You see that this is perfectly symmetric in the Fourier domain. That is certainly not the case with most of the orthogonal and biorthogonal wavelets, like the 'db' family. In those cases, scale to frequency is not so well defined because the wavelet is not symmetric in the Fourier domain and the bandwidth is much larger.

Also, in the new CWT we use L1 normalization which is much more natural in time-frequency analysis than the L2 normalization used in the older CWT. With L1 normalization, a sine wave of amplitude A, results in wavelet coefficients at the appropriate scale with magnitude A. In the older CWT, the magnitude of an oscillatory component in the wavelet coefficients depended on the scale.

We believe there are many other advantages of the new implementation in addition to the few I have mentioned. I would be very happy to discuss those and compare and contrast those at length with you.

Thank you again for your interest and for engaging in this way. As you said it is helpful for all.

Wayne

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Paramonte
on 13 Oct 2016

Edited: Paramonte
on 13 Oct 2016

Walter Roberson
on 13 Oct 2016

I disagree that users are "confused by having to specify scales"

Please remember the difference between "I find this easy to understand" and "Most users find this easy to understand" and "All users find this easy to understand".

Uneducated person: "Heavy objects fall faster than light objects" (gravity is misunderstood)

Grade school / high school / most undergraduates: "Gravity is easy, it is just a constant acceleration"

Quantum theorist / theoretical astrophysicist: "Gravity is one of the most mysterious forces in the Universe. Some of the best minds in the world have been trying to figure out gravity for the last hundred years, and there is so much we don't understand about it!"

SamIAm
on 25 Jan 2018

As someone who has recently learned about wavelets and started using them: Specifying scales was confusing, but I easily found references and learned how to do it for wavelets I had clear descriptions of. 'voices per octave', on the other hand, took me a lot of digging and trial and error to find info on. I still haven't found sufficient descriptions of exactly how the Morse wavelets are parameterized by matlab, and what the defaults are. I'm less bothered by the new version of cwt than I am extremely frustrated by the lack of detail and clarity in the documentation. For instance, I did not realize until this post that the old version was called if I gave different inputs to the function call, nor that the old version used L2 and the new version L1. I knew something screwy was going on with the normalization but couldn't figure out what. Is there a list of all the available Name-Value argument pairs somewhere? A list of all values you can get returned, and how they relate to the default plot matlab makes?

I know there was a helper function for plotting the output from the old cwt, and I was trying to use that to figure out how to interpret the output of the new cwt, but have yet to successfully make a similar plot manually (which I was trying to do in part to verify that I understood the autoplot and return values quantitatively).

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