Radar Reflectivity and Altitude Distributions of Lightning as a Function of IC, CG, and HY Flashes: Implications for LNOx Production. Issue 22 (25th November 2018)

• Record Type: Journal Article
• Authors: Mecikalski, Retha M.; Carey, Lawrence D.
• Is Part Of: Journal of geophysical research. Volume 123:Issue 22(2018)
• Page Start: 12, 796
• Page End: 12, 813
• Publication Date: 2018-11-25
• Subjects: lightning -- flash type -- altitude -- radar reflectivity -- storm type; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1029/2018JD029263
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: Two dimensional (2‐D) histogram distributions of lightning flashes relative to radar reflectivity and altitude were created using a total of 41, 180 intercloud/intracloud (IC) flashes, 3, 326 cloud‐to‐ground (CG) flashes, and 4, 349 hybrid (HY) flashes that originated in multicells; 111, 479 IC flashes, 8, 588 CG flashes, and 11, 699 HY flashes that originated in mesoscale convective systems; and 91, 283 IC flashes, 3, 023 CG flashes, and 7, 872 HY flashes that originated in supercells that occurred over northern Alabama and southern Tennessee. It was shown that although CG flashes initiate and propagate at the same altitude irrespective of storm type, IC flashes could have differences of up to 10 °C, while for HY flashes these differences increased to up to 20 °C relative to storm type. Further, IC, CG, and HY flashes propagated in lower reflectivities than where they initiated, while CG flashes initiated and propagated within higher reflectivities than IC and HY flashes. HY flashes were also twice as large as IC flashes and ~40% larger than CG flashes, and flashes that originated in mesoscale convective systems had larger overall sizes as compared to multicells and supercells. When comparing the new 2‐D histogram distributions to the legacy distributions used for the calculation of lightning‐produced nitrogen oxides (LNOx), it was shown that the new distributions perform much better, with higher Pearson product moment correlation coefficient values and much lower root‐mean‐square errors. These new distributions are thus more appropriate to use when modeling LNOx and will lead to more accurate LNOx estimations than using the legacy distributions. Key Points: Two‐dimensional radar reflectivity and altitude distributions of intercloud/intracloud, cloud‐to‐ground, and hybrid flashes vary with storm type The new altitude and reflectivity distributions of lightning by flash and storm types are more accurate than the legacy approach Flash sizes vary as a function of flash type and storm type with hybrid flashes having the largest sizes, irrespective of storm type