Estimation of convective rainfall from lightning observations

Citation
A. Tapia et al., Estimation of convective rainfall from lightning observations, J APPL MET, 37(11), 1998, pp. 1497-1509
Citations number
48
Categorie Soggetti
Earth Sciences
Journal title
JOURNAL OF APPLIED METEOROLOGY
ISSN journal
08948763 → ACNP
Volume
37
Issue
11
Year of publication
1998
Pages
1497 - 1509
Database
ISI
SICI code
0894-8763(199811)37:11<1497:EOCRFL>2.0.ZU;2-R
Abstract
The objective of this study is to develop a technique to use lightning obse rvations for estimating convective rainfall. A framework for rainfall estim ation is developed in which key elements are 1) the rainfall-lightning rati o, that is, the convective rainfall mass per cloud-to-ground lightning flas h; 2) the spatial distribution of rainfall relative to flash locations; and 3) the temporal distribution of rainfall relative to the time of lightning occurrence. These three elements are examined through a study of 22 summer thunderstorms in the domain covered by the Melbourne, Florida, WSR-88D rad ar during August of 1992 and 1993. The analyses are carried out by combinin g lightning observations from the National Lightning Detection Network with storm parameters computed from 3D reflectivity observations using the Thun derstorm Identification Tracking and Nowcasting storm-tracking and analysis algorithms. The effect of the prevailing convective regime on the variabil ity of lightning-rainfall relationships is investigated. The rainfall estim ation procedure is implemented and tested for a thunderstorm that occurred on 20 August 1992. Striking similarities in the spatial distribution of rai nfall estimates are observed for the rainfall maps derived from lightning o bservations and those derived from WSR-88D reflectivity observations. Rainf all estimates derived from lightning observations are of potential use for short-term prediction of flash floods, especially in regions of poor radar coverage; Potential uses of this method also include correction of radar-es timated rainfall for range effects.