04.04.2015 Views

Phase and Amplitude Variation in Montreal Weather

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Registration<br />

• Let the unconstra<strong>in</strong>ed smooth be x(t) <strong>and</strong><br />

the strictly periodic smooth be x 0 (t).<br />

• We need to estimate a nonl<strong>in</strong>ear strictly<br />

<strong>in</strong>creas<strong>in</strong>g smooth transformation of time<br />

h(t), called a warp<strong>in</strong>g function, , such that<br />

a fitt<strong>in</strong>g criterion is m<strong>in</strong>imized.

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