Abstract

As convective clouds in Northeast Asia are accompanied by various hazards related with heavy rainfall and thunderstorms, it is very important to detect convective initiation (CI) in the region in order to mitigate damage by such hazards. In this study, a novel approach for CI detection using images from Meteorological Imager (MI), a payload of the Communication, Ocean, and Meteorological Satellite (COMS), was developed by improving the criteria of the interest fields of Rapidly Developing Cumulus Areas (RDCA) derivation algorithm, an official CI detection algorithm for Multi-functional Transport SATellite-2 (MTSAT-2), based on three machine learning approaches—decision trees (DT), random forest (RF), and support vector machines (SVM). CI was defined as clouds within a 16 × 16 km window with the first detection of lightning occurrence at the center. A total of nine interest fields derived from visible, water vapor, and two thermal infrared images of MI obtained 15–75 min before the lightning occurrence were used as input variables for CI detection. RF produced slightly higher performance (probability of detection (POD) of 75.5% and false alarm rate (FAR) of 46.2%) than DT (POD of 70.7% and FAR of 46.6%) for detection of CI caused by migrating frontal cyclones and unstable atmosphere. SVM resulted in relatively poor performance with very high FAR ~83.3%. The averaged lead times of CI detection based on the DT and RF models were 36.8 and 37.7 min, respectively. This implies that CI over Northeast Asia can be forecasted ~30–45 min in advance using COMS MI data.

Highlights

  • Convective clouds are developed by various weather systems such as meso-scale convective systems, migrating frontal cyclones, and large-scale monsoonal fronts, which often result in heavy rainfall and thunderstorm events [1,2,3,4,5]

  • Setvak and Doswell III [17] used an infrared channel of Advanced Very High Resolution Radiometer (AVHRR) to detect convective storms by assuming that the tops of convective storms are composed of ice cloud particles only and they can be characterized as blackbodies

  • The p-values in each box plot were derived by t-tests of the convective initiation (CI) and non-CI samples of the interest field at the 95% confidence level

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Summary

Introduction

Convective clouds are developed by various weather systems such as meso-scale convective systems, migrating frontal cyclones, and large-scale monsoonal fronts, which often result in heavy rainfall and thunderstorm events [1,2,3,4,5]. Various meteorological hazards, such as lightning, hail, gusty winds, and floods, are closely related to heavy rainfall and thunderstorms accompanied by convective clouds [3,6,7,8,9,10]. Yuan and Li [18] extracted convective clouds using cloud optical depth and TB obtained from the infrared channels of Moderate

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