We study the initial downward propagation of long sprite streamers in naturally varying air density with numerical simulations on adaptively refined grids. We find that the ionization rate and the light emission from the streamer head increase approximately linearly with air density (therefore exponentially with time) while the radius hardly changes, in contradiction with a naive application of scaling laws. Charge conservation creates a negative charge and a consecutively enhanced electric field in the upper section of the streamer channel, while the head carries a growing positive charge. The high electric field in the upper part of the channel generates a secondary ionization wave and a luminous trail. The negative charging explains...
We investigate the launch of negative upward streamers from sprite glows. This phenomenon is readily...
We simulate short positive and negative streamers in air at standard temperature and pressure. First...
It is by now well understood that large sprite discharges at the low air densities of the mesosphere...
We study the initial downward propagation of long sprite streamers in naturally varying air density ...
Sprite discharges above thunderclouds at altitudes of 40-90 km (refs 1-5) are usually created by a s...
We simulate short positive and negative streamers in air at standard temperature and pressure. First...
We investigate the launch of negative upward streamers from sprite glows. This phenomenon is readily...
International audience[1] The lightning current waveforms observed simultaneously with high-speed vi...
The complex dynamics of a sprite discharge are not limited to the propagation of streamers. After th...
International audienceCarrot sprites, exhibiting both upward and downward propagating streamers, and...
It is by now well understood that large sprite discharges at the low air densities of the mesosphere...
[1] We study the electrical conductivity of a sprite streamer channel at three different altitudes (...
We investigate the launch of negative upward streamers from sprite glows. This phenomenon is readily...
We simulate short positive and negative streamers in air at standard temperature and pressure. First...
It is by now well understood that large sprite discharges at the low air densities of the mesosphere...
We study the initial downward propagation of long sprite streamers in naturally varying air density ...
Sprite discharges above thunderclouds at altitudes of 40-90 km (refs 1-5) are usually created by a s...
We simulate short positive and negative streamers in air at standard temperature and pressure. First...
We investigate the launch of negative upward streamers from sprite glows. This phenomenon is readily...
International audience[1] The lightning current waveforms observed simultaneously with high-speed vi...
The complex dynamics of a sprite discharge are not limited to the propagation of streamers. After th...
International audienceCarrot sprites, exhibiting both upward and downward propagating streamers, and...
It is by now well understood that large sprite discharges at the low air densities of the mesosphere...
[1] We study the electrical conductivity of a sprite streamer channel at three different altitudes (...
We investigate the launch of negative upward streamers from sprite glows. This phenomenon is readily...
We simulate short positive and negative streamers in air at standard temperature and pressure. First...
It is by now well understood that large sprite discharges at the low air densities of the mesosphere...