Phase and Amplitude Variation in Montreal Weather
Phase and Amplitude Variation in Montreal Weather
Phase and Amplitude Variation in Montreal Weather
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The warp<strong>in</strong>g function h(t)<br />
Every smooth strictly monotone function<br />
h(t) such that h(0) = 0 can be<br />
represented as<br />
t<br />
ht () C exp wvdvdu ( )<br />
u<br />
= ∫ ∫<br />
0 0<br />
We represent unconstra<strong>in</strong>ed function<br />
w(v) by a B-spl<strong>in</strong>e expansion. Constant<br />
C is determ<strong>in</strong>ed by constra<strong>in</strong>t h(T) = T.