Thunderstorm Characteristics during the Ontario Winter Lake-Effect Systems Project

• Published in: Journal of applied meteorology and climatology Vol. 57; no. 4; pp. 853 - 874
• Main Authors: Steiger, Scott M., Kranz, Tyler, Letcher, Theodore W.
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01-04-2018
• Subjects: Aircraft; Antennas; Boundary layer stability; Boundary layers; Case depth; Cloud-to-ground lightning; Clouds; Detection; Electric fields; Instability; Kinematics; Lakes; Lightning; Lightning detection; Microphysics; Remote sensing; Snowstorms; Stability; Storms; Thunderstorms; Turbine engines; Turbines; Wind power; Wind turbines; Winter; New York; Canada; Ontario Canada; Lake Ontario; United States > US
• ISSN: 1558-8424; 1558-8432
• DOI: 10.1175/JAMC-D-17-0188.1

The Ontario Winter Lake-Effect Systems (OWLeS) field campaign during the winter season of 2013/14 provided unprecedented data with regard to the structure and behavior of long-lake-axis-parallel (LLAP) lake-effect storms. One of the interesting characteristics of LLAP storm bands is their ability to initiate lightning. The OWLeS datasets provide an opportunity to examine more thoroughly the kinematics and microphysics of lake-effect thunder-snowstorms than ever before. The OWLeS facilities and field personnel observed six lake-effect thunderstorms during December–January 2013/14. Most of them produced very little lightning (fewer than six cloud-to-ground strokes or intracloud pulses recorded by the National Lightning Detection Network). The 7 January 2014 storm had over 50 strokes and pulses, however, which resulted in 20 flashes over a 6-h period (0630–1230 UTC), making it the most electrically active storm during the field campaign. Relative to the 18 December 2013 storm, which only had three flashes, the 7 January 2014 case had a deeper boundary layer and greater instability. Also, 45% of the lightning during the 7 January storm was likely due to flashes initiated by wind turbines or other man-made antennas, along with all of the lightning observed during 18 December. No lightning was documented over Lake Ontario, the primary source of instability for these storms.