4.3 Article

The RELAMPAGO Lightning Mapping Array: Overview and Initial Comparison with the Geostationary Lightning Mapper

Journal

JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
Volume 37, Issue 8, Pages 1457-1475

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JTECH-D-20-0005.1

Keywords

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Funding

  1. Instituto Nacional de Tecnologia Agropecuaria (INTA)
  2. FAMAF-UNC
  3. U.S. Department of Energy (DOE)
  4. NASA MSFC Shipping and Receiving
  5. NASA [80NSSC18K1689]
  6. Serena Group
  7. U.S. Embassy in Argentina
  8. NOAA GOES-R Program
  9. NASA Lightning Imaging Sensor (LIS) project
  10. NASA MSFC Award [NNM11AA01A]
  11. NSF
  12. NSF Research Experience for Undergraduates (REU) program
  13. NASA [NNM11AA01A, 146621] Funding Source: Federal RePORTER

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During November 2018-April 2019, an 11-station very high frequency (VHF) Lightning Mapping Array (LMA) was deployed to Cordoba Province, Argentina. The purpose of the LMA was validation of the Geostationary Lightning Mapper (GLM), but the deployment was coordinated with two field campaigns. The LMA observed 2.9 million flashes ( >= five sources) during 163 days, and level-1 (VHF locations), level-2 (flashes classified), and level-3 (gridded products) datasets have been made public. The network's performance allows scientifically useful analysis within 100 km when at least seven stations were active. Careful analysis beyond 100 km is also possible. The LMA dataset includes many examples of intense storms with extremely high flash rates (>1 s(-1)), electrical discharges in overshooting tops (OTs), as well as anomalously charged thunderstorms with low-altitude lightning. The modal flash altitude was 10 km, but many flashes occurred at very high altitude (15-20 km). There were also anomalous and stratiform flashes near 5-7 km in altitude. Most flashes were small (<50 km(2) area). Comparisons with GLM on 14 and 20 December 2018 indicated that GLM most successfully detected larger flashes (i.e., more than 100 VHF sources), with detection efficiency (DE) up to 90%. However, GLM DE was reduced for flashes that were smaller or that occurred lower in the cloud (e.g., near 6-km altitude). GLM DE also was reduced during a period of OT electrical discharges. Overall, GLM DE was a strong function of thunderstorm evolution and the dominant characteristics of the lightning it produced.

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