Abstract
Dual-polarized coherent radar measurements are used to estimate the differential propagation phase φDP between horizontal and vertical polarization states. The slope of φDP is an estimate of the specific differential phase KDP. This process is complicated due to differential phase on backscatter δ between horizontal and vertical polarization states, which can be signficiant at C band. Filtering techniques are presented for separating δ from propagation phase and then estimating KDP and δ. Also discussed are procedures for the estimation and interpretation of other radar measureables such as conventional radar reflectivity, differential reflectivity ZDR, the magnitude of the copolar correlation coefficient ρHV(0), and Doppler spectrum width σv. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 155-164 |
| Number of pages | 10 |
| Journal | Journal of Atmospheric and Oceanic Technology |
| Volume | 10 |
| Issue number | 2 |
| DOIs | |
| State | Published - 1993 |