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A full analysis of this feature is difficult and requires the replacement of e- λ2 t in Eq. 1 with (1-a) e- λ2 t +a e- λ3 t cos (2πνt), where a (1) is an amplitude and λ3 is a large relaxation rate. Since this approach does not alter our interpretation we do not pursue it here.
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A full analysis of this feature is difficult and requires the replacement of e- λ2 t in Eq. 1 with (1-a) e- λ2 t +a e- λ3 t cos (2πνt), where a (1) is an amplitude and λ3 is a large relaxation rate. Since this approach does not alter our interpretation we do not pursue it here.
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