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Detailed Reference Information |
Füllekrug, M., Ignaccolo, M. and Kuvshinov, A. (2006). Stratospheric Joule heating by lightning continuing current inferred from radio remote sensing. Radio Science 41: doi: 10.1029/2006RS003472. issn: 0048-6604. |
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The mean lightning current waveform of particularly intense lightning discharges is inferred from 52,510 radio wave recordings in the frequency range 1--200 Hz. The current waveform decays initially with a time constant of ~2 ms, and the current lowers ~60 C from cloud to ground within the first ~10 ms of the discharge. The subsequent continuing current exhibits a decay time constant of ~40 ms and lowers ~170 C from cloud to ground within the next ~100 ms of the discharge. The total charge transfer ~230 C from cloud to ground deposits electrical energy into the stratosphere resulting from quasi-static (Joule) heating. The energy deposition is dominated by the lightning continuing current, and it is ~10-5 J/m3 at 30 km height. It is speculated that the initiation of blue jets and gigantic jets in the stratosphere may result from lightning continuing current $gtrsim$100 ms which can be observed with radio waves at frequencies $lesssim$10 Hz. |
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BACKGROUND DATA FILES |
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Abstract![](/images/icons/spacer.gif) |
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Keywords
Electromagnetics, Wave propagation (2487, 3285, 4275, 4455, 6934), Geomagnetism and Paleomagnetism, Rapid time variations, Atmospheric Processes, Atmospheric electricity, Atmospheric Processes, Lightning, Radio Science, Electromagnetic noise and interference |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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