Polarimetric radar characteristics of lightning initiation and propagating channels

In this paper we present an analysis of a large dataset of lightning and polarimetric weather radar data collected in the course of a lightning measurement campaign that took place in the summer of 2017 in the area surrounding Säntis, in the northeastern part of Switzerland. For this campaign and fo...

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Bibliographic Details
Authors: Figueras i Ventura, Jordi; Pineda Rüegg, Nicolau|||0000-0002-2507-8424; Besic, Nikola; Grazioli, Jacopo; Hering, Alessandro; Van der Velde, Oscar Arnoud|||0000-0002-1638-6628; Romero Durán, David|||0000-0002-5571-9069; Sunjerga, A.; Mostajabi, A.; Azadifar, M.; Rubinstein, M.; Montañá Puig, Juan|||0000-0003-2488-697X; Germann, Urs; Rachidi-Haeri, Farhad
Format: Article
Publication date:2019
Country:España
Institution:Universitat Politècnica de Catalunya (UPC)
Repository:UPCommons. Portal del coneixement obert de la UPC
Language:English
OAI Identifier:oai:upcommons.upc.edu:2117/134831
Online Access:https://hdl.handle.net/2117/134831
https://dx.doi.org/10.5194/amt-12-2881-2019
Access Level:Open access
Keyword:Atmospheric physics
Lightning Mapping Array
lightning
thunderstorms
radar
upward lightning
polarimetric radar
Santïs
Física atmosfèrica
Àrees temàtiques de la UPC::Enginyeria elèctrica
Description
Summary:In this paper we present an analysis of a large dataset of lightning and polarimetric weather radar data collected in the course of a lightning measurement campaign that took place in the summer of 2017 in the area surrounding Säntis, in the northeastern part of Switzerland. For this campaign and for the first time in the Alps, a lightning mapping array (LMA) was deployed. The main objective of the campaign was to study the atmospheric conditions leading to lightning production with a particular focus on the lightning discharges generated due to the presence of the 124¿m tall Säntis telecommunications tower. In this paper we relate LMA very high frequency (VHF) sources data with co-located radar data in order to characterise the main features (location, timing, polarimetric signatures, etc.) of both the flash origin and its propagation path. We provide this type of analysis first for all of the data and then we separate the datasets into intra-cloud and cloud-to-ground flashes (and within this category positive and negative flashes) and also upward lightning. We show that polarimetric weather radar data can be helpful in determining regions where lightning is more likely to occur but that lightning climatology and/or knowledge of the orography and man-made structures is also relevant.