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Polarimetric and Electrical Characteristics of a Lightning Ring in a Supercell Storm
by
MacGorman, Donald R.
, Biggerstaff, Michael I.
, Kuhlman, Kristin M.
, Schuur, Terry J.
, Rust, W. David
, Payne, Clark D.
in
Atmospheric electricity
/ Atmospheric research
/ C band
/ Climatology
/ Correlation coefficient
/ Correlation coefficients
/ Density
/ Doppler sonar
/ Downdraft
/ Earth, ocean, space
/ Electrification
/ Exact sciences and technology
/ External geophysics
/ Graupel
/ Instrumentation
/ Instruments
/ Investigations
/ Kinematics
/ Lightning
/ Lightning activity
/ Meteorology
/ Polarimetric radar
/ Polarimetry
/ Radar
/ Reflectance
/ Severe storms
/ Signatures
/ Storms
/ Storms, hurricanes, tornadoes, thunderstorms
/ Studies
/ Surveillance radar
/ Telex
/ Thunderstorms
/ Tornadoes
/ Universal time
/ Updraft
/ Vertical vorticity
/ Vorticity
/ Water in the atmosphere (humidity, clouds, evaporation, precipitation)
/ Weather
2010
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Polarimetric and Electrical Characteristics of a Lightning Ring in a Supercell Storm
by
MacGorman, Donald R.
, Biggerstaff, Michael I.
, Kuhlman, Kristin M.
, Schuur, Terry J.
, Rust, W. David
, Payne, Clark D.
in
Atmospheric electricity
/ Atmospheric research
/ C band
/ Climatology
/ Correlation coefficient
/ Correlation coefficients
/ Density
/ Doppler sonar
/ Downdraft
/ Earth, ocean, space
/ Electrification
/ Exact sciences and technology
/ External geophysics
/ Graupel
/ Instrumentation
/ Instruments
/ Investigations
/ Kinematics
/ Lightning
/ Lightning activity
/ Meteorology
/ Polarimetric radar
/ Polarimetry
/ Radar
/ Reflectance
/ Severe storms
/ Signatures
/ Storms
/ Storms, hurricanes, tornadoes, thunderstorms
/ Studies
/ Surveillance radar
/ Telex
/ Thunderstorms
/ Tornadoes
/ Universal time
/ Updraft
/ Vertical vorticity
/ Vorticity
/ Water in the atmosphere (humidity, clouds, evaporation, precipitation)
/ Weather
2010
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Polarimetric and Electrical Characteristics of a Lightning Ring in a Supercell Storm
by
MacGorman, Donald R.
, Biggerstaff, Michael I.
, Kuhlman, Kristin M.
, Schuur, Terry J.
, Rust, W. David
, Payne, Clark D.
in
Atmospheric electricity
/ Atmospheric research
/ C band
/ Climatology
/ Correlation coefficient
/ Correlation coefficients
/ Density
/ Doppler sonar
/ Downdraft
/ Earth, ocean, space
/ Electrification
/ Exact sciences and technology
/ External geophysics
/ Graupel
/ Instrumentation
/ Instruments
/ Investigations
/ Kinematics
/ Lightning
/ Lightning activity
/ Meteorology
/ Polarimetric radar
/ Polarimetry
/ Radar
/ Reflectance
/ Severe storms
/ Signatures
/ Storms
/ Storms, hurricanes, tornadoes, thunderstorms
/ Studies
/ Surveillance radar
/ Telex
/ Thunderstorms
/ Tornadoes
/ Universal time
/ Updraft
/ Vertical vorticity
/ Vorticity
/ Water in the atmosphere (humidity, clouds, evaporation, precipitation)
/ Weather
2010
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Polarimetric and Electrical Characteristics of a Lightning Ring in a Supercell Storm
Journal Article
Polarimetric and Electrical Characteristics of a Lightning Ring in a Supercell Storm
2010
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Overview
On 30 May 2004, a supercell storm was sampled by a suite of instrumentation that had been deployed as part of the Thunderstorm Electrification and Lightning Experiment (TELEX). The instrumentation included the Oklahoma Lightning Mapping Array (OK-LMA), the National Severe Storms Laboratory S-band Weather Surveillance Radar-1988 Doppler (WSR-88D) polarimetric radar at Norman, Oklahoma, and two mobile C-band, Shared Mobile Atmospheric Research and Teaching Radars (SMART-R). Combined, datasets collected by these instruments provided a unique opportunity to investigate the possible relationships among the supercell’s kinematic, microphysical, and electrical characteristics. This study focuses on the evolution of a ring of lightning activity that formed near the main updraft at approximately 0012 UTC, matured near 0039 UTC, and collapsed near 0050 UTC. During this time period, an F2-intensity tornado occurred near the lightning-ring region. Lightning density contours computed over 1-km layers are overlaid on polarimetric and dual-Doppler data to assess the low- and midlevel kinematic and microphysical characteristics within the lightning-ring region. Results indicate that the lightning ring begins in the middle and upper levels of the precipitation-cascade region, which is characterized by inferred graupel. The second time period shows that the lightning source densities take on a horizontal u-shaped pattern that is collocated with midlevel differential reflectivity and correlation coefficient rings and with the strong cyclonic vertical vorticity noted in the dual-Doppler data. The final time period shows dissipation of the u-shaped pattern and the polarimetric signatures as well as an increase in the lightning activity at the lower levels associated with the development of the rear-flank downdraft (RFD) and the envelopment of the vertical vorticity maximum by the RFD.
Publisher
American Meteorological Society
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