Prof. Nesbitt will be participating in a webinar on 9/11/13 sponsored by PBS/NOVA and the National Earth Science Teachers Association. Click here for more information!
It is a common practice with SIGMET signal processors (and even from other radars such as research radars and operational data such as NEXRAD) to use the Doppler velocity spectrum in an attempt to filter ground clutter from other fields (which ideally has a near 0 velocity spectrum). Clutter (reflections off of objects, both stationary and moving targets such as mountains, aircraft, buildings, cars, etc.) is an annoyance because it contaminates the presentation of the radar images as well as causes errors in radar retrievals (velocity for severe weather interpretation, precipitation estimates, etc.). One idea is to remove the clutter by filtering the time series (pulse by pulse) by removing returns with near zero velocity. This is desirable because the remaining signal will be meteorological echo (which is usually moving towards or away from the radar). However, sometimes it’s not, and here are some examples where it can cause problems.
Here is an example from a NEXRAD PPI near Cleveland in widespread precipitation (snow in this case), showing the reduction in reflectivity factor near the radar where the velocity is near 0. You can see this effect nearly every time there is stratiform rain near a NEXRAD. The algorithm must have a range or altitude dependence, since the effect usually goes away after 15 km or so. However, if you’re trying to use reflectivity to estimate precipitation, the value of Z is missing some meteorological echo. It’s probably better than possibly including clutter (which will blow up your estimates of precipitation or mean particle size), but not ideal.
The problem is that this removes power from meteorological echo, and thus can bias Z and Zdr measurements in these regions. Here is an example of this in action: in this RHI scan a 0 isodop (an isodop is a surface of constant Doppler velocity) filter is able to remove low level clutter, but also removes valid data near the 0 isodop. When designing radar scanning strategies, the radar meteorologist must be aware of these settings for each sweep, and for research measurements it may be advisable to use polarimetric methods of QC rather than using the velocity spectra.
In this animation, you can see that in the “quality controlled” reflectivity (the image without the clutter and clear air echo aloft, there is power missing where the mean Doppler velocity is near 0 (especially below the freezing level in several broad horizontal regions), as shown via the black areas in the image below:
It also influences the differential reflectivity (Zdr), making the values negative since more power is preferentially removed from the horizontal reflectivity compared with the vertical reflectivity:
Online publication date: 1-Jul-2009.
Abstract . Full Text . PDF (2852 KB)
and there is even a patent on the technique outlined in the first paper! It is not known at this time what specific filtering technique was used on the data displayed here. The impact is the following: The “quality controlled” reflectivity field, and other fields are impacted with biases, that must be identified and removed from quantitative retrievals. In addition, this quality control process deleted data in many of the other fields, which along with biases in the measured fields hampers the use of dual-polarization variables for quality control (including correlation coefficient and standard deviation of differential propagation phase). We have the uncorrected reflectivity, but we can’t effectively use the polarimetric variables to correct the This cannot be undone in recorded data, so unless one is careful, this issue can cause issues with your dataset.
Carey, L. D., S. A. Rutledge, D. A. Ahijevych, and T. D. Keenan, 2000: Correcting propagation effects in C-band polarimetric radar observations of tropical convection using differential propagation phase. J. Appl. Meteor., 39, 1405–1433. [Abstract]
Clearly improving time series/spectral analysis is an active area of research, so stay tuned for improved algorithms. Note that dual-pol QC methods aren’t perfect either, but that topic will be saved for another post.
Software credit: ARM-PyART, Argonne National Lab
We’ve added a new page with a small but hopefully growing list of radar data resources. Stay tuned for updates!
It was recently announced that a group led by Prof. Steve Nesbitt in the Atmospheric Sciences department including Prof. Greg McFarquhar and research scientist Dr. Brian Jewett has been selected to the NASA Precipitation Measurement Missions (PMM) Science Team for 2013-2016. This project will involve our group in the Global Precipitation Measurement (GPM) mission satellite project, which is set to launch in early 2014. This project will involve the validation and improvement of the algorithms that go into retrieving precipitation rates globally from space, including participation in upcoming field projects in Iowa and the mountains of North Carolina.