In some of my efforts to fill in missing data with **entropy** criteria,
I have often based the entropy on the **spectrum**
and then found that the **envelope** would misbehave.
I have come to believe that the definition of entropy
should involve both the spectrum and the envelope.
To get started,
let us assume that the power of a seismic signal is the product
of an envelope function times a spectral function,
say

(20) |

(21) | ||

(22) | ||

(23) | ||

(24) | ||

(25) |

It is remarkable that all the cross terms have disappeared and that the resulting entropy is the sum of the two parts.

Now we will tackle the same calculation with the geometric inequality:

(26) | ||

(27) | ||

(28) | ||

(29) | ||

(30) |

Again all the cross terms disappear, and the resulting entropy is the sum of the two parts. I wonder if this result applies for the other Jensen inequalities.

In conclusion, although this book is dominated by model building using the method of least squares, Jensen inequalities suggest many interesting alternatives.

10/21/1998