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Performance characteristics of the NLDN for return strokes and pulses superimposed on steady currents, based on rocket‐triggered lightning data acquired in Florida in 2004–2012
Author(s) -
Mallick S.,
Rakov V. A.,
Hill J. D.,
Ngin T.,
Gamerota W. R.,
Pilkey J. T.,
Biagi C. J.,
Jordan D. M.,
Uman M. A.,
Cramer J. A.,
Nag A.
Publication year - 2014
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2013jd021401
Subject(s) - lightning detection , lightning (connector) , peak current , rocket (weapon) , environmental science , meteorology , physics , geology , remote sensing , thunderstorm , engineering , aerospace engineering , quantum mechanics , power (physics) , electrode , electrochemistry
We present a detailed evaluation of performance characteristics of the U.S. National Lightning Detection Network (NLDN) using, as ground truth, Florida rocket‐triggered lightning data acquired in 2004–2012. The overall data set includes 78 flashes containing both the initial stage and leader/return‐stroke sequences and 2 flashes composed of the initial stage only. In these 80 flashes, there are a total of 326 return strokes (directly measured channel‐base currents are available for 290 of them) and 173 kiloampere‐scale (≥1 kA) superimposed pulses, including 58 initial continuous current pulses and 115 M components. All these events transported negative charge to the ground. The NLDN detected 245 return strokes and 9 superimposed pulses. The resultant NLDN flash detection efficiency is 94%, return‐stroke detection efficiency is 75%, and detection efficiency for superimposed pulses is 5% for peak currents ≥1 kA and 32% for peak currents ≥5 kA. For return strokes, the median location error is 334 m and the median value of absolute peak current estimation error is 14%. The percentage of misclassified events is 4%, all of them being return strokes. The median value of absolute event‐time mismatch (the difference in times at which the event is reported to occur by the NLDN and recorded at the lightning triggering facility) for return strokes is 2.8 µs. For two out of the nine superimposed pulses detected by the NLDN, we found optical evidence of a reilluminated branch (recoil leader) coming in contact with the existing grounded channel at an altitude of a few hundred meters above ground.