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A frontal thunderstorm with several multi-cell lines found to produce energetic preliminary breakdown

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F22%3A00553343" target="_blank" >RIV/68378289:_____/22:00553343 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216208:11320/22:10456488

  • Result on the web

    <a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021JD035780" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2021JD035780</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1029/2021JD035780" target="_blank" >10.1029/2021JD035780</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    A frontal thunderstorm with several multi-cell lines found to produce energetic preliminary breakdown

  • Original language description

    We combine electromagnetic measurements with meteorological and lightning detection data to explain an observation of unusually strong preliminary breakdown (PB) produced by a thunderstorm system that developed along the Mediterranean Coast of Southern France in the early hours of 19 June 2013. This multi-cellular storm was composed of several parallel convective lines in the NW-SE direction. Our analysis focuses on ten sequences of energetic electromagnetic PB pulses recorded by two receivers located at different distances from this thunderstorm. The peak currents, which generated these strong PB pulses, reached -36 kA. The initial polarity of all observed energetic PB pulses confirmed the movement of the negative charge downward, as in case of PB pulses preceding negative cloud-to-ground discharges. The locations of PB pulses appeared in areas with none or very weak lightning activity. Most PB pulses were initiated in small, short-living, rapidly moving convective storm cells characterized by low reflectivity values (generally < 40 dBZ), weak vertical development, and low flash density. Our findings indicate that the observed thunderstorm might posses temporary strong negatively charged pockets located above a strong positive charge region at low-level. Such charge arrangement, likely explains our observation of unusually strong PB pulses and the absence of RS pulses in electromagnetic recordings.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10305 - Fluids and plasma physics (including surface physics)

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2022

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Journal of Geophysical Research-Atmospheres

  • ISSN

    2169-897X

  • e-ISSN

    2169-8996

  • Volume of the periodical

    127

  • Issue of the periodical within the volume

    4

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    18

  • Pages from-to

    e2021JD035780

  • UT code for WoS article

    000765621000003

  • EID of the result in the Scopus database

    2-s2.0-85125151250