Evolution of global lightning in the transition from cold to warm phase preceding two super El Niño events

Williams, E.; Bozóki, T.; Sátori, G.; Price, C.; Steinbach, P.; Guha, A.; Liu, Y.; Beggan, C.D.; Neska, M.; Boldi, R.; Atkinson, M.. 2021 Evolution of global lightning in the transition from cold to warm phase preceding two super El Niño events. Journal of Geophysical Research: Atmospheres, 126 (3), e2020JD033526. https://doi.org/10.1029/2020JD033526

Before downloading, please read NORA policies.

Preview

Text
2020JD033526.pdf - Published Version
Available under License Creative Commons Attribution Non-commercial No Derivatives 4.0.
Download (9MB) | Preview

Official URL: http://dx.doi.org/10.1029/2020JD033526

Abstract/Summary

Multi-station observations of Schumann resonance (SR) intensity document common behavior in the evolution of continental-scale lightning activity in two super El Niño events, occurring in 1997/98 and 2015/16. The vertical electric field component of SR at Nagycenk, Hungary and the two horizontal magnetic field components in Rhode Island, USA in 1997, and in 2014–2015, the two horizontal magnetic field components at Hornsund, Svalbard and Eskdalemuir, United Kingdom as well as in Boulder Creek, California and Alberta, Canada exhibit considerable increases in SR intensity from some tens of percent up to a few hundred percents in the transition months preceding the two super El Niño events. The UT time distribution of anomalies in SR intensity indicates that in 1997 the lightning activity increases mainly in Southeast Asia, the Maritime Continent and India, i.e. the Asian chimney region. On the other hand, a global response in lightning is indicated by the anomalies in SR intensity in 2014 and 2015. SR-based results are strengthened by comparison to independent lightning observations from the Optical Transient Detector and the World Wide Lightning Location Network, which also exhibit increased lightning activity in the transition months. The increased lightning is attributable to increased instability due to thermodynamic disequilibrium between the surface and the mid-troposphere during the transition. The main conclusion is that variations in SR intensity may act as a precursor for the occurrence and magnitude of these extreme climate events, and in keeping with earlier findings, as a precursor to maxima in global surface air temperature.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1029/2020JD033526
ISSN:	2169-897X
Date made live:	08 Feb 2021 13:54 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/529580

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1029/2020JD033526

ISSN:

2169-897X

Date made live:

08 Feb 2021 13:54 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/529580