| (8.68) |
where
is the complex conjugate of
.
An analogous characterization of the covariance between two variables X
and Y is:
| (8.69) |
where
and
are the Fourier transforms of the functions X(t) and Y(t).
Unlike the variance spectrum,
has both real and imaginary parts, which are called respectively the cospectrum
and the quadrature spectrum
:
| (8.70) |
The cospectrum often finds application in atmospheric research because it characterizes the contributions to a product from different frequencies. For example, the cospectrum of vertical wind and water vapor density shows the contributions to the vertical flux of water vapor from different wavelength components in a turbulent field.
Two other functions that can be determined from
and
are
the squared coherence spectrum
and
the phase spectrum
:
| (8.71) |
and
| (8.72) |
where the overbars denote averages over some frequency interval and
and
are the variance spectra for X and Y, respectively. Because
the equation for the coherence is identically unity for any individual
frequency, averaging of nearby estimates is necessary if these results
are to be meaningful. After such averaging, the coherence can be used to
test for consistency in the phase relationship between the two variables.
If the phases change randomly for components in the selected interval,
the coherence will tend to zero as the number of estimates increases. If
there is coherence between the two variables, the phase function characterizes
the phase between the two components.