Using Lightning as a HF Signal Source to Produce Ionograms

Modern techniques for specifying the ionosphere include the use of ionosondes, which both transmit and receive sweep soundings in the high‐frequency (HF) band. We replicate this process by observing the broad band emission from lightning using the Long Wavelength Array, Sevilleta, radio telescope. W...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Radio science 2018-11, Vol.53 (11), p.1419-1425
Hauptverfasser: Obenberger, K. S., Dowell, J. D., Malins, J., Parris, R. T., Pedersen, T. R., Taylor, G. B.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Modern techniques for specifying the ionosphere include the use of ionosondes, which both transmit and receive sweep soundings in the high‐frequency (HF) band. We replicate this process by observing the broad band emission from lightning using the Long Wavelength Array, Sevilleta, radio telescope. We use this station to observe the powerful broadband radio bursts from the breakdown of air that occurs during lightning flashes. For nearby lightning we observe both the direct line of sight and the delayed ionospheric reflection. By correlating the amplitude time series from the direct line of sight to that of the ionospheric reflection, we can accurately measure the group delay as a function of frequency. By separating into right‐hand circular and left‐hand circular, we can derive both the O mode and X mode ionograms. This novel technique allows for accurate ionograms to be made even in restricted frequency bands and provides a means to probe density profiles at multiple locations of the ionosphere on short time scales with a single receiver station. Plain Language Summary In this paper, we present a novel technique that leverages the natural radio emissions from lightning as a signal source to measure the electron density profile of the bottomside ionosphere. Such profile measurements are known as ionograms. Previous methods to produce ionograms make use of RADAR systems composed of both a transmitter and receiver. Our method, however, requires only a receiver placed in proximity to ongoing lightning storms. These measurements are the first of their kind to use naturally occurring radio emission to produce ionograms. This work opens the door to further research, where scattered storms could provide key measurements for specifying the spatial and temporal structure present within the ionosphere. Key Points Lightning generates the required signal needed for ionospheric specification The ionograms presented here are the first to be derived from lightning measurements Measurements are not subject to frequency restrictions
ISSN:0048-6604
1944-799X
DOI:10.1029/2018RS006680