Jeff Snyder
EF5
This will be a very nice upgrade to the current radars. The shape (and therefore type) of the hydrometeor will be able to be determined and radar rainfall estimates should improve. As of now, when high reflectivity values are seen, one cannot be sure if heavy rain or hail exists in that region. With dual-polarimetric radar we will be able to combine dBZ and ZDR (differential reflectivity) values to determine what type of precip is occurring.
Don't forget about rho_hv, which is very helpful in terms of determining hydrometeor classes. Additionally, KDP serves an important purpose as well, even outside of QPE.
Honestly, I think for many chasers (both in the field and armchair) the recent super-res upgrade is bigger than the DP upgrade will be. The one exception I can think of is what RDale brought up -- the tornado debris signature. However, we don't really have a good gauge on how "common" this signature is since there are only a handful of polarimetric weather radars that have sampled tornadic supercells. Having worked with X-band polarimetric data for the past few years, I think availability of polarimetric data from the WSR88D network is going to be confusing and not particularly useful for the vast majority of casual radar observers. Nearly all of us on this forum can interpret ZH and Vr imagery, but adding more variables (KDP, RHOhv, ZDR) can greatly complicate the interpretation of the data. In fact, I'm not sure the additional data are going to be very useful for most folks, particularly in a real-time situation with casual interrogation. Of course, for op mets or those who want to interrogate intensely a storm, the additional data will often be extremely useful.
For those who are interested in the , the paper outlining the WSR88D hydrometeor classification scheme was recently published in Wea. and Forecasting:
Park, S-G, A. V. Ryzhkov, D. S. Zrnić, and K-E Kim, 2009: The hydrometeor classification algorithm for the polarimetric WSR-88D: Description and application to an MCS. Wea. and Forecasting, 24, 730-748.
I'll point out the following to interested readers:
Kumjian, M., and A. V. Ryzhkov, 2008: Polarimetric signatures in supercell thunderstorms. J. Appl. Met., 47, 1940-1961.
Kumjian, M., and A. V. Ryzhkov, 2009: Storm-relative helicity revealed from polarimetric radar observations. J. Atmos. Sci., 66, 667-685.
Romine, G. S., D. W. Burgess, and R. B. Wilhelmson, 2008: A dual-polarization-radar-based assessment of the 8 May 2003 Oklahoma City area tornadic supercell. Mon. Wea. Rev., 136, 2849-2870.
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