Improved rainfall estimates in convective storms using polarisation diversity radar

Citation
Aj. Illingworth et al., Improved rainfall estimates in convective storms using polarisation diversity radar, HYDROL E S, 4(4), 2000, pp. 555-563
Citations number
40
Categorie Soggetti
Earth Sciences
Journal title
HYDROLOGY AND EARTH SYSTEM SCIENCES
ISSN journal
10275606 → ACNP
Volume
4
Issue
4
Year of publication
2000
Pages
555 - 563
Database
ISI
SICI code
1027-5606(200012)4:4<555:IREICS>2.0.ZU;2-#
Abstract
Errors arise when using conventional radar reflectivity, Z, to estimate rai nfall rate, R,and these can be particularly severe during severe convective storms; the very events when accurate estimates are needed so that action can be taken to mitigate the effects of flooding. Concentration is on three problems associated with heavy rainfall: hail, attenuation and absolute ca libration of the radar, and consider how polarisation radar parameters, dif ferential reflectivity, Z(DR), and specific differential phase shift K-DP, might lead to their alleviation. It is essential to consider the fundamenta l limits to the accuracy with which these parameters can be estimated. If Z DR can be measured to an accuracy of 0.2 dB, then it provides a measure of mean raindrop shape which is sufficiently precise to improve rainrate estim ates. This can be achieved at S-band (10 cm), but seems very difficult for operational C-band (5 cm) radars; differential attenuation by the heavy rai n introduces a negative bias into Z(DR) which increases with range. However , the magnitude of this bias at C-band can then be used to correct for the total attenuation of Z. Differential phase, K-DP, has the advantage that it is a phase measurement and so is unaffected by attenuation. It only respon ds to the rainfall and is unaffected by the hail, but K-DP is a noisy param eter and is only useful for heavy rainfall above 30-60 mm hr(-1). Fortuitou sly, K-DP and Z(DR) are not independent and one use of K-DP and Z(DR) may w ell be to exploit this redundancy to identify rain areas as opposed to hail , and in rainfall to use the redundancy to provide an automatic calibration of the absolute reflectivity, Z, to 0.5 dB (12%). Finally, the noisy chara cter of both ZDR and KDP together with the low level of the co-polar correl ation coefficient provide the first reliable means of detecting and removin g anomalous propagation which is a major operational problem for all weathe r radars.