Abstract

Abstract. In this paper, recent changes to the Meteosat thunderstorm TRacking And Monitoring algorithm (Cb-TRAM) are presented as well as a validation of Cb-TRAM against data from the European ground-based LIghtning NETwork (LINET) of Nowcast GmbH and the South African Weather Service Lightning Detection Network (SAWS LDN). Validation is conducted along the well-known skill measures probability of detection (POD) and false alarm ratio (FAR) on the basis of Meteosat/SEVIRI pixels as well as on the basis of thunderstorm objects. The values obtained demonstrate specific limitations of Cb-TRAM, as well as limitations of satellite methods in general which are based on thermal emission and solar reflectivity information from thunderstorm cloud tops. Although the climatic conditions and the occurrence of thunderstorms are quite different for Europe and South Africa, quality score values are similar. Our conclusion is that Cb-TRAM provides robust results of well-defined quality for very different climatic regimes. The POD for a thunderstorm with intense lightning is about 80% during the day. The FAR for a Cb-TRAM detection which is not even close to intense lightning is about 50%. If only proximity to any lightning activity is required, FAR is much lower at about 15%. Pixel-based analysis shows that detected thunderstorm object size is not indiscriminately large, but well within physical limitations of the satellite method. Night-time POD and FAR are somewhat worse as the detection scheme does not use the high-resolution visible information during night-time hours. Nowcasting scores show useful values up to approximately 30 min in advance.

Highlights

  • Hydrology and Earth System basis of Meteosat/SEVIRI pixels as well as on the basis of Sciences thunderstorm objects

  • We presented a comparison of Meteosat-based thunderstorm detection and short-term forecasts with ground-based lightning data. This way a validation of the Cb-TRAM (Thunderstorm Tracking and Monitoring) algorithm for the detection of mature thunderstorms against lightning ground-truth is provided over 6 months in two different regions of the world (Europe and South Africa)

  • The validation is conducted by evaluation of probability of detection (POD) and false alarm ratio (FAR) for different lightning intensity classes and different spatial accuracy requirements

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Summary

Introduction

Hydrology and Earth System basis of Meteosat/SEVIRI pixels as well as on the basis of Sciences thunderstorm objects. The values obtained demonstrate spe- In recent years a wide range of possibilities for thunderstorm cific limitations of Cb-TRAM, as well as limitations of satel- nowcasting based on satellite data have become available, lite methods in general which are based on thermal emis- due to the temporal and spatial coverage especially from sion and solar reflectivity information from thunderstorm cloud tops. The climatic conditions and the occurrence of fraRed Imager). The Cb-TRAM (Cumulonimbus Tracking thunderstorms are quite different for Europe and South and Monitoring) algorithm of the German Aerospace Cen-. Cb-TRAM provides robust results of well-defined quality for multi-channel Meteosat SEVIRI data (Zinner et al, 2008).

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