Calibrating Differential Reflectivity on the WSR-88D

Dusan S. Zrnic NOAA/National Severe Storms Laboratory, Norman, Oklahoma

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Valery M. Melnikov Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, and NOAA/OAR/National Severe Storms Laboratory, Norman, Oklahoma

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John K. Carter Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, and NOAA/OAR/National Severe Storms Laboratory, Norman, Oklahoma

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Abstract

A calibration procedure of differential reflectivity on the Weather Surveillance Radar-1988 Doppler (WSR-88D) is described. It has been tested on NOAA's modified WSR-88D research and development polarimetric radar and is directly applicable to radars that simultaneously transmit and receive waves having horizontal and vertical polarization.

Corresponding author address: Dusan Zrnic, NOAA/Severe Storms Laboratory, 1313 Halley Circle, Norman, OK 73069. Email: dusan.zrnic@noaa.gov

Abstract

A calibration procedure of differential reflectivity on the Weather Surveillance Radar-1988 Doppler (WSR-88D) is described. It has been tested on NOAA's modified WSR-88D research and development polarimetric radar and is directly applicable to radars that simultaneously transmit and receive waves having horizontal and vertical polarization.

Corresponding author address: Dusan Zrnic, NOAA/Severe Storms Laboratory, 1313 Halley Circle, Norman, OK 73069. Email: dusan.zrnic@noaa.gov

1. Introduction

On polarimetric radars that transmit simultaneous horizontal and vertical polarizations three variables must be calibrated. These are reflectivity factor, differential reflectivity, and differential phase. Reflectivity factor remains the most difficult and elusive. Differential phase is not calibrated per se; rather the system differential phase is measured to determine the beginning of the phase unwrapping interval (Zahrai and Zrnic 1993). This can be done by equating the mean phase of ground clutter to the system differential phase (Zrnic et al. 2006). Differential reflectivity ZDR does need to be calibrated with special care; for example, the rainfall estimator tested by Ryzhkov et al. (2005) has a bias error of 18% if the bias of ZDR is 0.2 dB.

Hubbert et al. (2003) suggest a way to calibrate differential reflectivity using natural scatterers. The method is well suited for fully polarimetric radars, that is, those that measure all the elements of the backscatter covariance matrix. Its essence is to use sun scan for calibrating the receiving path and cross-polar measurement for calibrating the transmit path including the transmitted powers. Ryzhkov et al. (2005) also relied on the sun scan for calibrating ZDR in the receiver chain and propose measurement in dry aggregates at high elevation angles for complete transmit–receive calibration.

Soon the national network of Weather Surveillance Radar-1988 Doppler (WSR-88D) radars will be fitted with the polarimetric capability. Calibration of differential reflectivity on the network presents a couple of challenges. First, immediately after retrofitting any of the radars to dual polarization the differential reflectivity should be properly calibrated. Second, calibration should be maintained at all times during operations. This paper suggests how to meet these two calibration requirements on the WSR-88D network. Section 2 describes the systems' hardware pertinent for calibration. The step-by-step procedure is explained in section 3, whereas sections 4 and 5 present measurements in the transmitter and receiver chains of the research WSR-88D radar. Constraints and assumptions are also listed.

2. Calibration ports on the radar system

In developing the procedure we set the following goals. 1) Existing parts and capabilities of the current WSR-88D should be used; this eliminates calibration at vertical incidence, or addition of extra hardware beyond at most one mechanical microwave switch. 2) Calibration must be possible immediately after retrofitting radar; this eliminates reliance on precipitation. 3) Calibration should be over the full dynamic range; this enlists the need for a variable attenuator. 4) There should be no temporal drift in the calibration curve over several volume scans; this demands calibration at the end of each volume scan.

The block diagram in Fig. 1 captures the gist of the research and development radar on which the procedure has been tested. The radar (KOUN) is a modified version of WSR-88D such that it can simultaneously transmit and receive horizontally and vertically polarized waves. It serves as proof of concept for polarimetric development of the WSR-88Ds and has a digital receiver (RVP8 processor; Sigmet 2005) with a 72-MHz sampling rate that will be standard on the operational network. Thus the future dual-polarization WSR-88Ds will be very similar to the KOUN, and the procedure developed herein is directly applicable to radars on the network.

The points labeled 1–4 in Fig. 1 are relevant for the subsequent discussion. Point 1 represents the coupler for transmitter power measurement. Points 2 are two couplers above the elevation rotary joints (EL) for power measurements. The baseline WSR-88D calibration method used these power monitors, but the performance was not satisfactory. The latest versions of the WSR-88D, which are fitted with the Open Radar Data Acquisition System (ORDA), do not use these monitors although the hardware remains in place. The production design for the polarimetric WSR-88D will likely include improved measurement of the transmitted power. Point S is near the antenna plane just outside of the radome and indicates the sun's radiation flux. Points 3 correspond to calibration couplers near the input to the low noise amplifiers (LNAs). In each channel between point 3 and the LNA there is a waveguide filter (bandwidth ∼16 MHz) and receiver protector that are not drawn in Fig. 1. Points 4 represent outputs of the digital receivers, one in the channel for horizontal (H) polarization, and the other in the channel for vertical (V) polarization. These outputs are in-phase and quadrature phase (I, Q) values of H and V components from which various powers, noises, and differential reflectivity are computed.

For calibrating reflectivity and instantaneous gains and phases of the automatic gain control the WSR-88D has a special circuit (Fig. 1, left part with the RF continuous wave and noise generators, and the variable attenuator), which, as will be demonstrated here, is crucial for maintaining calibrated ZDR. The built-in variable attenuator (Fig. 1) can be changed in steps of 1 dB over a 103-dB range. Under computer control it connects to one of the four internal sources (three are shown in Fig. 1); the continuous wave (CW) generator and noise generator are pertinent for calibrating ZDR. After the attenuator the signal is directed by a switch to either the input of the LNA (points 3 in Fig. 1) or the input to the first mixer (not shown), or it is disabled.

The gains and attenuations in the H and V channels differ and cause bias of differential reflectivity. The essence behind the procedure is to partition calibration into parts that measure constant system biases (such as the ones caused by waveguides and power splitter) and parts that measure time-varying biases (such as in active circuits). The time-invariant parts are measured once to establish the constant bias. The slowly varying bias is tracked over the full dynamic range from volume scan to volume scan analogous to calibration of the automatic gain control (AGC) circuit on the WSR-88Ds. Initially, the sun scan is used to determine the two-way bias between the elevation rotary joints and the space outside the radome (Melnikov et al. 2003).

The basic assumption for calibration is that the time constant of the slow drift is considerably longer than the duration of volume scan. This is needed to ensure that correction for bias from volume scan to volume scan can be made. Further, measurements on various contributors of constant bias are sequential and some involve common paths, so we assume that the bias does not change between such measurements. This assumption must be checked by immediately repeating the measurements that have a common path; that is what we did and recommend to others. Second, the sun's radiation is randomly polarized so that the horizontal and vertical components have equal mean powers. We have verified that this holds by making the measurements over a long period of time.

Bias between any two points is denoted with the symbol Δij, where the first subscript (i) is the input point and the second (j) is the output. Although Δij = Δji, some of the biases can be easily measured in one direction but not in the opposite because of the placement of couplers and signal flow direction. In general the signal flow direction both during measurement and actual operation is from the port indicated by the first index. Unless stated otherwise, the bias is expressed in decibels.

3. Bias measurement procedure

The calibration consists of separate measurements of the constant bias ΔC and the time-varying bias Δ34, which are summed to obtain the total bias. At the end of each volume scan the time-varying part should be updated. The constant bias must be measured initially and should be checked occasionally after changes on the system have been made, or during periodic maintenance. On the KOUN we do not automatically update the time-varying part but make a manual correction at the start of data collection. Nonetheless, we present herein the reasons for automatic update and demonstrate, via repetitive measurements over several hours, that it is sound.

The fixed bias from transmission and back to the calibration ports (3, Fig. 1) is
i1520-0426-23-7-944-e1
where ΔS2 is the bias between the EL joint (at ports 2 in Fig. 1) and the antenna output referred to outside of radome (Fig. 1). The factor 2 accounts for the two-way path (transmit and receive). The imbalance in transmitted powers at the elevation joints is denoted by Δ12, and Δ23 is the bias between the elevation joints and the input to the LNA. Constant bias ΔC is time invariant because it is caused by fixed passive components. We have determined that it is independent of the angular positions of the rotary joints (i.e., changes are smaller than 0.01 dB). The remaining bias Δ34 from calibration ports (3 in Fig. 1) to output of digital receiver is caused by the two active receiver paths (input to the LNA, mixers, and amplifiers). It varies with time and might depend on the received power. Thus ΔC is added to the variable bias to obtain the total bias.
Here Δ12 is directly measured, whereas ΔS2 and Δ23 are measured indirectly as
i1520-0426-23-7-944-e2
i1520-0426-23-7-944-e3
where Δ34 is measured using an external signal generator as described in section 5c. Bias Δ34 is measured using the internal generator (Fig. 1), which is under computer control; hence the measurement is fast and nonintrusive. But, because the differential gains might change in time, measurement of Δ23 consists of three steps. First, we measure Δ34, then Δ23, and then again Δ34; if the Δ34 does not change, the measurement is valid, otherwise it is repeated until a change smaller than a tolerable error is obtained. Similarly, any measurement from points other than 3 to 4 (output of the digital receiver) must be bracketed by a measurement from points 3 to 4. This type of differential measurement has another advantage in that only the input point of measurement changes while the output is always the digital receiver, so the intrusion into the system is minimal.

We set out to achieve an overall error smaller than 0.1 dB; therefore (assuming independent errors), a desirable value for the error in one measurement is about 0.04 dB so that the cumulative rms error of the four measurements is about 0.08 dB.

Note that the expression for ΔS2 consists of four terms that could be reduced to two but are not. The reason is to avoid the deleterious effects of time variations. That is, measure Δ34, then ΔS4, and then Δ34; if the two measurements of Δ34 agree within 0.03 dB, we accept the ΔS4. Therefore, ΔS4 − Δ34 is measured in three steps and so is Δ24 − Δ34.

4. Measurement of constant bias in transmission chain

Waveguides were opened at the elevation rotary joints (points 2, Fig. 1). Power was injected at the coupler (point 1, Fig. 1) just above the transmitter. The difference (H power – V power) at the output of the two waveguides was about 0.04 dB (i.e., the bias Δ12 = −0.04 dB). This value is also the smallest that we can discern on the power meter; hence the error in measurement could be at most 0.04 dB. We measured and recorded the coupling losses; these agreed exactly with the values stamped by the manufacturer. Therefore, on similar high-quality radars measurement can be done at the couplers' outputs as explained in the following paragraph.

The waveguides were properly connected, the transmitter was turned on, and measurements were made at the couplers above the elevation rotary joints. For safety it may be wise to reduce the transmitter power by 10 or 20 dB, which we have not done on the KOUN. Because the measurements were made sequentially, we have recorded the transmitter power during each measurement. This is highly recommended. The difference of losses between the H and V channels was 0.06 dB (H had higher loss), in excellent agreement with the measurement on open waveguides. Thus we record Δ12 = −0.06 dB.

The combined specified loss (not measured by us) of the coupler above the elevation joints and the path to the feed horn for the vertical and horizontal channels is 0.2 dB. Therefore, the bias between the two channels must be much smaller than 0.2 dB and is deemed excellent. Nonetheless, there could be a differential gain of the antenna at two polarizations and minute differential loss through the radome. Measurements from sun scan are needed to estimate the total effect.

5. Measurements of bias in the receiving chain

Herein described are measurements of the variable bias, the fixed bias, and the receiver noise in the two channels. For ZDR calibration no absolute value of power is needed, but the changes in relative values of power at the digital receiver output must be known. Measurements are differential in nature and all the comparisons are done by using digital powers in arbitrary units at the output of the digital receiver.

a. Receiver noise levels in the two channels

This is straightforward. It requires the antenna to be pointed high into the sky away from the ground. The two noise powers Nh and Nv should be recorded. On the KOUN, Nh = −113 dBm and Nv = −114 dBm. We recommend that the noise powers be estimated on each individual radial of data using spectral analysis and/or range locations where the signal is absent. This would improve differential reflectivity estimates at low signal-to-noise ratios (SNRs) by properly accounting for noise variability. Causes of this variability include outside interferences, radiation from precipitation along the beam, lighting, radiation of the ground, which is intercepted by antenna sidelobes, and so on.

b. Variable bias (Δ34)

As stated in section 3, the total bias Δ consists of two parts, long-term stable ΔC and the slowly changing part Δ34, mainly due to drifts in the amplifiers of the two channels. At different powers of the digital receiver output the bias can have different values; therefore, we explicitly introduce this power Phk (in arbitrary units) to the argument of the bias. The subscript “h” indicates horizontal polarization and k indicates power levels (i.e., setting of the attenuator). Thus,
i1520-0426-23-7-944-e4
In the argument of Δ34, Phk is given by
i1520-0426-23-7-944-e5
that is, the noise is subtracted from the power at the output of the digital receiver. The units of powers in (5) are internal to the RVP8.

The variable bias needs to be measured over the full dynamic range of the receiver (i.e., for the full range of H powers Phk measured at the digital receiver output) at the end of each volume scan. This has not been done on the KOUN although stepping of the attenuation is automated and time series data are recorded from which the bias can be computed. Further, we have semiautomated the procedure to step automatically through all settings of the attenuator.

The bias curve Δ34(Phk) in Fig. 2 is computed as
i1520-0426-23-7-944-e6
where the index k refers to the sequence of output power changes (corresponding to 2-dB attenuation steps), h and v refer to the polarization channels in the digital receiver, and the signal and noise powers are estimates from time series data.

In Fig. 2 two curves are shown, the noise-corrected one [as in (6)], which supposedly should be applicable, and the curve for which the noise has not been subtracted on the right-hand side of Eq. (6); in both cases power Ph in the abscissa has no noise. Rather than straightening the bias cure, the noise correction at low SNRs (∼0 dB) is in the wrong direction. We have determined that the cause is coherent leakage in the internal CW frequency generator, which is present only when this generator is connected to make the calibration; it affects the output at high attenuator settings for which the SNR < 30 dB.

At the high end of dynamic range the departure from the constant value is due to saturation effects. Otherwise, the curve is flat down to about −55 dB. From there on the departure above the constant value is caused by the coherent leakage. This we have established by measurements with an external generator (Fig. 3), with the internal noise generator (Fig. 4), and by spectral analysis. Maximum variation in the flat part is about 0.02 dB. The fact that the curve is flat indicates that the gain characteristics of the two receivers are well matched and the gains are offset by a fixed amount. It will shortly be shown that the good match extends to low signals as well; hence it suffices to extrapolate the bias to the low end of dynamic range.

c. Difference in receiver chain from EL couplers to the calibration port 23)

Two measurements are needed to obtain Δ23. These are measurement of Δ24 and measurement of Δ34 at the same output signal power. Then
i1520-0426-23-7-944-e7
is the difference bias. On the KOUN we recorded time series data to obtain the values.

Output power from a CW signal (HP generator) was split and injected at the couplers above the elevation rotary joints (ports 2 in Fig. 1) to obtain the bias Δ24(Ph) in Fig. 3. Here Ph is the power (horizontal channel) at the output of digital receiver in arbitrary units internal to the processor. The SNRh = 0 dB corresponds to –113 dBm, referred to the LNA input. In Ph on the abscissa the noise power Nh has been subtracted; that is, Ph = PhtotalNh. Two bias curves are shown; in one the noises Nh and Nv have been subtracted from Ph and Pv to compute the bias; in the other they have not. This is to illustrate the match between the two channels and to determine the value at which receivers' noises begin to influence the measurement. Definitely the noise-corrected bias is constant and reliable down to –5 dB of SNR; beyond, the bias correction is futile because estimates of differential reflectivity would be dominated by uncertainty in measurements.

In Fig. 3 Δ24(Ph) covers a much larger dynamic range than needed for determining this constant bias. It suffices to make measurements at few values in the middle of the dynamic range (anywhere between −40 and −60 dB in Fig. 3) and average the result.

d. Difference from the outside of radome to EL couplers S2)

This measurement also requires two steps and use of previously determined value of Δ23. The equation is
i1520-0426-23-7-944-e8
Note that ΔS4 is measured with the sun scan, and Δ34(Ng) must be measured with the internal noise generator. To distinguish the Δ34 measured with internal noise generator we have included (Ng) in parentheses. There are two reasons why the noise generator is used. 1) The sun and noise generator are broad band as is the weather signal, whereas the signal generator is narrow band. The two receivers might not be identical: there is the obvious difference of gains that is calibrated with the narrowband CW generator, but the small difference of integrated powers (over all frequencies) of broadband signals could be of the order of 0.1 dB (no such difference was found on the KOUN). 2) On the KOUN there is a coherent leakage signal if the internal CW generator is connected; it affects measurements at SNR < 30 dB. No coherent leakage signal is present if the internal noise generator is connected.

To measure Δ34(Ng) we use the internal noise generator and built-in attenuator in the range from 0 to 20 dB; this results in an output signal (from the noise generator) to receiver noise ratio of 22 to 2 dB. In the same round we repeated the noise measurements Nh and Nv by increasing the attenuation to a very large value (>80 dB).

The Δ34(Nghk) measured on the KOUN is plotted in Fig. 4. For the noise-corrected curve the receiver noise powers were subtracted before computation, but in either case the noise generator power on the abscissa Ng = PhtotalNh, where Phtotal is the estimate at the output of digital receiver and Nh is the receiver noise power estimate (also at output of digital receiver).

The noise-corrected bias (Fig. 4) is fairly uniform down to the SNRh = 0 dB. The change thereafter might be due to small coherent leakage and noise. Because the power from the sun is typically between −75 and −80 units, the measurement (on the KOUN) is not sensitive to these effects.

To determine total receiver bias we scanned the antenna over a small sector at an elevation close to the elevation of the sun. We let the sun drift through the scanning plane and record ΔS4 (that is ZDR) and Ph (see Fig. 5). The peak of Ph indicates that the sun is centered on the beam. There will be several peaks (Fig. 5) as the sun enters the plane of the scan. The highest of the peaks is identified and differential reflectivity is computed (after subtracting Nh and Nv, which are estimated at the end of sun scan) for that point and all the points up to 2 dB below it. The average of these values is the differential reflectivity bias ΔS4.

Plotted in Fig. 5 are Ph and Pv (in linear units at the output of digital receiver) and differential reflectivity bias ΔS4 (dotted curve). The noises Nh and Nv have not been subtracted in any of these plots, but have been accounted for in the listed results. One can see that the bias is near −0.6 dB. At the time of about 310 s there is a sharp increase of differential reflectivity and drop in signal powers. This is when we began receiver noise measurement. Clearly, the difference in noise powers between the two receivers causes discontinuity in differential reflectivity. In the KOUN case the SNR from the sun scan is typically 10 dB.

To give readers a feel of the stability of the measured bias using the sun (noise corrected), we list (Table 1) values obtained over about 1 h of time on 11 March 2005 (same day as for data in Fig. 5). Noises have been subtracted to compute ΔS4. The rms deviation about the mean (∼−0.62 dB) of these measurements is 0.025 dB.

The estimated values of ΔS4 and Δ34(Ng = Psun) are substituted into (8) to obtain the bias ΔS2. Because the Δ34(Ng) is available in discrete increments, one might need to interpolate to obtain the Δ34(Ng = Psun) at the power corresponding to the power from the sun.

Next, in Fig. 6 we present ΔS3 = ΔS4 – Δ34 obtained over a 5-month period from March until July of 2005. The sun scan measurement was preceded with the “before” and followed by “after” measurement of Δ34 using the noise generator. The time between two measurements with the noise generator was about 10 min. Note the remarkable stability of the difference ΔS4 – Δ34. The mean value is ΔS3 = −0.30 dB; the standard deviation = 0.028 dB might be caused by variations in the polarization of sun's radiation or in the position of the rotary joints. In all but two cases there were no changes in the “before” and “after” values of Δ34.

e. Summary of measurements

We have obtained the following values for the constant parts of bias: Δ12 = −0.06 dB, Δ23 = −0.36 dB, ΔS3 = −0.3 dB, and ΔS2 = ΔS3 − Δ23 = 0.06 dB. Therefore, the total constant bias (1) is ΔC = −0.3 dB.

It turns out that over a large dynamic range the variable bias Δ34(Ph) is independent of power Ph but does change in time (this is why the bias in Figs. 2 –4 might seem inconsistent). Therefore, on the KOUN and similar radars this bias can be measured at a strong power and the values can be extrapolated to smaller powers. Such extrapolation is straight if the change of Δ34(Ph) is a linear function of Ph. At the time of these measurements (March 2005) typical values on the KOUN were between −0.4 and −0.5 dB, so that the bias correction was an addition of 0.7 to 0.8 dB.

A key to successful bias correction is to automatically track the temporal variation of Δ34 and make corrections from volume scan to volume scan. The variations of Δ34 can be significant with occasional large (0.7 dB) abrupt changes as seen in Fig. 7. Such an abrupt change would be missed in one volume scan so that the ZDR could be that much off. Nonetheless, calibration for the subsequent volume scan would redress this fault.

We have found significant coherent leakage at SNRs < 30 dB if the internal CW signal generator is applied to the calibration's port. Because the voltage of the CW generator and the leakage voltage add the effect on bias measurement is very strong, much more so than if the powers were additive. Rather than fight this problem we have found a way around it that is robust, repeatable, and produces differential reflectivity with error smaller than 0.1 dB. This error is a conservative estimate that assumes 0.04 dB of independent error for each of the four bias components; the transmitted power at elevation coupler has an error of about 0.04 dB, and the errors in the other three bias components are kept at 0.03 dB. We have no independent verification of the accuracy, but values of differential reflectivity in regions of light aggregates above the melting layer are consistent with the calibrated ZDR and very often agree within 0.1 dB. Disagreements we attribute to the time variation of gains in the two receiver chains. Clearly, the automatic procedure advocated herein is needed to have continuously superior calibration.

6. Conclusions

A procedure for calibrating differential reflectivity has been developed and tested on the KOUN polarimetric radar. At its essence is separation of the bias into a constant part and time-varying part (due to active receiver components). It proceeds as follows.

  • Constant part is measured at the time of radar installation and at times when pertinent components are replaced; it is due to the transmitter path and part of the receiver path.

  • Transmitter path is measured at the couplers above the elevation rotary joints using the transmitted signal.

  • Receiver path consists of two pairs of measurements. One pair uses internal noise generator, sun scan, and again the noise generator to establish the difference between the outside of radome and the LNAs inputs. The other pair uses the internal CW generator, external signal generator, and again the internal CW generator to measure the difference between the elevation rotary joints and the LNAs inputs.

  • From the differences in the receiver path one computes the part between the elevation rotary joints and the outside of radome.

  • The time-varying part must be updated at the end of each volume scan.

  • The total bias is the sum of constant and time-varying parts.

Overall there are four sets of measurements, one in the transmission path and three in the receiving path. We have shown that each of the sets has an rms error smaller than 0.04 dB; hence the total is less than 0.08 dB.

The recommended procedure can achieve errors within 0.1 dB, if caution and care is exercised such that 1) all differences in coupling losses are accounted for, 2) noises are correctly estimated and subtracted from the H and V powers, 3) some measurements are repeated or bracketed by a companion measurement, and 4) high-quality equipment is used.

Assuming that the quality of upgraded WSR-88D is equal or better than that of the KOUN, the procedure tested herein is directly transferable. Nonetheless, there may be residual problems of a practical nature in perfecting the technique on any radar network. Most measurements can be automated under computer control. This applies to those with internal CW and noise generators, and to sun scans. Measurement with the external generator attached to couplers above the EL rotary joints can be semiautomated so that the results from the output of the digital receiver are readily available.

Because absolute calibration of reflectivity within 1 dB is still hard to achieve it will appear to casual readers that our claim of 0.1-dB accuracy is exaggerated. The principal reason that this is not so is in the relative comparisons of the two channels. Because the transmitted power is split, on transmit the relative difference is constant; similarly, the relative difference in much of the receiver path is constant and what remains is to continuously track the relative difference in the receiver gains.

Acknowledgments

We thank Allen Zahrai for leading the team of engineers who designed the new processor and controls of the radar and oversaw subsequent modifications used herein. Igor Ivic gave valuable advice concerning coherent leakage. Mike Schmidt and Richard Wahkinney made extensive modifications of microwave circuitry and controls and actively participated in many measurements. We are also grateful to those that did not interfere. The reviewer's comments have been very helpful. Part of this work was supported by the National Weather Service, the Federal Aviation Administration, and the Air Force Weather Service through the NEXRAD Product Improvement Program. For Melnikov and Carter, funding was provided by NOAA/Office of Oceanic and Atmospheric Research under NOAA/University of Oklahoma Cooperative Agreement NA17RJ1227, U.S. Department of Commerce.

REFERENCES

  • Hubbert, J. C., Bringi V. N. , and Brunkow D. , 2003: Studies of the polarimetric covariance matrix. Part I: Calibration methodology. J. Atmos. Oceanic Technol, 20 , 696706.

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  • Melnikov, V. M., Zrnic D. S. , Doviak R. J. , and Carter J. K. , 2003: Calibration and Performance Analysis of NSSL's Polarimetric WSR-88D, NOAA/NSSL Report, 77 pp.

  • Ryzhkov, V. R., Giangrande S. E. , Melnikov V. M. , and Schuur T. J. , 2005: Calibration issues of dual-polarization radar measurements. J. Atmos. Oceanic Technol, 22 , 11381155.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Sigmet, cited. 2005: The RVP8™ Digital IF Receiver and Signal Processor: Overview, 2005. [Available online at http://www.sigmet.com.].

  • Zahrai, A., and Zrnic D. S. , 1993: The 10-cm-wavelength polarimetric weather radar at NOAA's National Severe Storms Laboratory. J. Atmos. Oceanic Technol, 10 , 649662.

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  • Zrnic, D. S., Melnikov V. M. , and Ryzhkov A. V. , 2006: Correlation coefficients between vertically and horizontally polarized returns from ground clutter. J. Atmos. Oceanic Technol, 23 , 381394.

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Fig. 1.
Fig. 1.

Diagram of the KOUN system with crucial points for calibrating differential reflectivity ZDR.

Citation: Journal of Atmospheric and Oceanic Technology 23, 7; 10.1175/JTECH1893.1

Fig. 2.
Fig. 2.

Bias Δ34 measured with the internal CW generator over the full dynamic range.

Citation: Journal of Atmospheric and Oceanic Technology 23, 7; 10.1175/JTECH1893.1

Fig. 3.
Fig. 3.

Bias Δ24 measured on the KOUN. The dashed line indicates receiver noise power (in internal relative RVP8 units).

Citation: Journal of Atmospheric and Oceanic Technology 23, 7; 10.1175/JTECH1893.1

Fig. 4.
Fig. 4.

Bias in differential reflectivity Δ34 measured with the internal noise generator. The receiver noise level Nh (subtracted from Phtotal) would correspond to −86.8 units.

Citation: Journal of Atmospheric and Oceanic Technology 23, 7; 10.1175/JTECH1893.1

Fig. 5.
Fig. 5.

Sun scan. Powers at horizontal and vertical polarizations (linear internal RVP8 units) and bias in differential reflectivity ΔS4. Noise powers have not been removed. The maximum signal to noise ratios are SNRh = 11.15 dB and SNRv = 12.07 dB, and the mean bias ΔS4 = −0.64 dB.

Citation: Journal of Atmospheric and Oceanic Technology 23, 7; 10.1175/JTECH1893.1

Fig. 6.
Fig. 6.

Measured bias from outside the radome to the calibration ports over a 5-month period.

Citation: Journal of Atmospheric and Oceanic Technology 23, 7; 10.1175/JTECH1893.1

Fig. 7.
Fig. 7.

Differential reflectivity bias between the LNAs and the digital receiver outputs vs time measured over a 10-h period on 26 Jun 2005.

Citation: Journal of Atmospheric and Oceanic Technology 23, 7; 10.1175/JTECH1893.1

Table 1.

Total receiver bias ΔS4 (from outside of radome to the output of the digital receiver) measured on 11 Mar 2005 over a period of 1 h.

Table 1.
Save
  • Hubbert, J. C., Bringi V. N. , and Brunkow D. , 2003: Studies of the polarimetric covariance matrix. Part I: Calibration methodology. J. Atmos. Oceanic Technol, 20 , 696706.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Melnikov, V. M., Zrnic D. S. , Doviak R. J. , and Carter J. K. , 2003: Calibration and Performance Analysis of NSSL's Polarimetric WSR-88D, NOAA/NSSL Report, 77 pp.

  • Ryzhkov, V. R., Giangrande S. E. , Melnikov V. M. , and Schuur T. J. , 2005: Calibration issues of dual-polarization radar measurements. J. Atmos. Oceanic Technol, 22 , 11381155.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Sigmet, cited. 2005: The RVP8™ Digital IF Receiver and Signal Processor: Overview, 2005. [Available online at http://www.sigmet.com.].

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  • Fig. 1.

    Diagram of the KOUN system with crucial points for calibrating differential reflectivity ZDR.

  • Fig. 2.

    Bias Δ34 measured with the internal CW generator over the full dynamic range.

  • Fig. 3.

    Bias Δ24 measured on the KOUN. The dashed line indicates receiver noise power (in internal relative RVP8 units).

  • Fig. 4.

    Bias in differential reflectivity Δ34 measured with the internal noise generator. The receiver noise level Nh (subtracted from Phtotal) would correspond to −86.8 units.

  • Fig. 5.

    Sun scan. Powers at horizontal and vertical polarizations (linear internal RVP8 units) and bias in differential reflectivity ΔS4. Noise powers have not been removed. The maximum signal to noise ratios are SNRh = 11.15 dB and SNRv = 12.07 dB, and the mean bias ΔS4 = −0.64 dB.

  • Fig. 6.

    Measured bias from outside the radome to the calibration ports over a 5-month period.

  • Fig. 7.

    Differential reflectivity bias between the LNAs and the digital receiver outputs vs time measured over a 10-h period on 26 Jun 2005.

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