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Multi-point Observation of Hiss Emerging from Lightning Whistlers
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We analyze continuous multi-point measurements of electromagnetic field
waveforms onboard the Cluster spacecraft in order to contribute to the
discussion on sources of plasmaspheric hiss, known as a shaping agent
for the Earth radiation belts. In our case study we aim at finding
sources of hiss observed close to the geomagnetic equator in the outer
plasmasphere on the dayside. We find hiss to be triggered from whistlers
of different spectral properties. Whistlers with the lowest observed
dispersion arrive to different spacecraft with time delays indicating
their origin in the northern hemisphere. Positions of source lightning
discharges are then found using the time coincidences with the Word Wide
Lightning Location Network data from three active thunderstorm regions
in Europe. We find that subionospheric propagation of lightning
atmospherics is necessary to explain the observations. Geographic
locations of their ionospheric exit points then determine spectral
properties of resulting unducted whistlers and triggered hiss. We
conclude that magnetospherically reflecting whistlers are a good
candidate for one of the embryonic sources of plasmaspheric hiss.
Title: Multi-point Observation of Hiss Emerging from Lightning Whistlers
Description:
We analyze continuous multi-point measurements of electromagnetic field
waveforms onboard the Cluster spacecraft in order to contribute to the
discussion on sources of plasmaspheric hiss, known as a shaping agent
for the Earth radiation belts.
In our case study we aim at finding
sources of hiss observed close to the geomagnetic equator in the outer
plasmasphere on the dayside.
We find hiss to be triggered from whistlers
of different spectral properties.
Whistlers with the lowest observed
dispersion arrive to different spacecraft with time delays indicating
their origin in the northern hemisphere.
Positions of source lightning
discharges are then found using the time coincidences with the Word Wide
Lightning Location Network data from three active thunderstorm regions
in Europe.
We find that subionospheric propagation of lightning
atmospherics is necessary to explain the observations.
Geographic
locations of their ionospheric exit points then determine spectral
properties of resulting unducted whistlers and triggered hiss.
We
conclude that magnetospherically reflecting whistlers are a good
candidate for one of the embryonic sources of plasmaspheric hiss.
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