Autocorrelation for moment estimations
The final spectrum moment calculation (for total power or SNR, mean velocity, and spectrum width) in all processing modes is based on autocorrelation moment estimation techniques.
Typically, the first three lags are
calculated, denoted as R0, R1 and
R2. There are two ways to calculate these, that is, time
domain or frequency domain calculation.
-
In the PPP mode for dual-polarization, the autocorrelations are computed directly in the time domain.
-
In DFT mode, they are computed by taking the inverse DFT of the Doppler power spectrum in the frequency domain.
In the DFT case, only the first 3 terms must be calculated.
The time domain and frequency domain techniques are nearly identical, except for that the method of taking the inverse DFT of the power spectrum relies on the assumption that the time series is periodic. Another difference is that for time domain calculation, only a rectangular weighting is used.
In the following table, M is the number of pulses in the time average. Here, s' denotes the clutter-filtered time series, s denotes the original unfiltered time series and the * denotes a complex conjugate. gr and gt represent the transmitter and receiver gains, that is, their product represents the total system gain.
| Parameter and definition | Physical model |
|---|---|
|
|
|
|
|
|
|
|
|
|
|
|
Since the RVP10 is a linear receiver, there
is a single gain number that relates the measured autocorrelation magnitude to the absolute
received power. However, since many of the algorithms do not require absolute calibration of
the power, the gain terms are ignored in the discussion of these.
To for the unfiltered time series is proportional to the sum
of the meteorological signal S, the clutter power
C and the noise power N. R0 is equal to
the sum of the meteorological signal S and noise power N
which is measured directly on the RVP10 by periodic noise sampling.
To and R0 are used for calculating
the dBZ values - the equivalent radar reflectivity factor which is a calibrated measurement.
The physical models for R0, R1 and
R2 correspond to a Gaussian weather signal and white noise.
W is the spectrum width and V' the mean
velocity, both for the normalized Nyquist interval on [-1 to 1].
The autocorrelation lags above and the
corresponding physical models have five unknowns: N, S,
C, V', W. Because the
R1 and R2 lags are complex, this
yields, effectively, 5 equations in 5 unknowns using the constraint provided by the argument
of R1. This closed system of equations can be solved for the
unknowns which is the basis for calculating the moments from the autocorrelations.
