Dm. Suszcynsky et al., FORTE observations of simultaneous VHF and optical emissions from lightning: Basic phenomenology, J GEO RES-A, 105(D2), 2000, pp. 2191-2201
Preliminary observations of simultaneous VHF and optical emissions from lig
htning as seen by the Fast on-Orbit Recording of Transient Events (FORTE) s
pacecraft are presented. VHF/optical waveform pairs are routinely collected
both as individual lightning events and as sequences of events associated
with cloud-to-ground (CG) and intracloud (IC) flashes. CG pulses can be dis
tinguished from IC pulses on the basis of the properties of the VHF and opt
ical waveforms but mostly on the basis of the associated VHF spectrograms.
The VHF spectrograms are very similar to previous ground-based HF and VHF o
bservations of lightning and show signatures associated with return strokes
, stepped and dart leaders, attachment processes, and intracloud activity.
For a typical IC flash, the FORTE-detected VHF is generally characterized b
y impulsive broadband bursts of emission, and the associated optical emissi
ons are often highly structured. For a typical initial return stroke, the F
ORTE-detected VHF is generated by the stepped leader, the attachment proces
s, and the actual return stroke. For a typical subsequent return stroke, th
e FORTE-detected VHF is mainly generated by dart leader processes. The dete
cted optical signal in both return stroke cases is primarily produced by th
e in-cloud portion of the discharge and lags the arrival of the correspondi
ng VHF emissions at the satellite by a mean value of 243 mu s. This delay i
s composed of a transit time delay (mean of 105 mu s) as the return stroke
current propagates from the attachment point up into the region of in-cloud
activity plus an additional delay due to the scattering of light during it
s traversal through the clouds. The broadening of the light pulse during it
s propagation through the clouds is measured and used to infer a mean of th
is scattering delay of about 138 mu s (41 km additional path length) for CG
light. This value for the mean scattering delay is consistent with the Tho
mason and Krider [1982] model for light propagation through clouds.