skip to main content
US FlagAn official website of the United States government
dot gov icon
Official websites use .gov
A .gov website belongs to an official government organization in the United States.
https lock icon
Secure .gov websites use HTTPS
A lock ( lock ) or https:// means you've safely connected to the .gov website. Share sensitive information only on official, secure websites.


Title: Three‐Dimensional Mapping of Lightning‐Produced Ionospheric Reflections
Abstract The powerful high‐frequency/very high frequency radio emissions that occur during lightning flashes can be used as a signal of opportunity to study the bottom side ionosphere. The lightning emission is bright, broad spectrum, and short in duration, providing an ideal signal of opportunity for making ionograms. This study continues previous work in Obenberger et al. (2018), where the direct line of sight signal from lightning can be cross correlated with megahertz frequency radio telescope observations to reveal ionogram traces created from the reflected lightning signals. This process was further developed to automate production of ionograms made from individual lightning flashes over the course of several hours, as well as create new techniques to detect the lightning signal using the all‐sky‐imaging mode. By using the Long Wavelength Array Sevilleta radio telescope as an interferometer, the point of reflection of the lightning signal for each frequency of the ionogram can be located in the ionosphere, instantaneously revealing density gradients within the ionosphere on minute time scales. We also explore the minimum size stations required for the application of this technique, which we found to be at least 32 antennas.  more » « less
Award ID(s):
1835400
PAR ID:
10458547
Author(s) / Creator(s):
 ;  ;  ;  
Publisher / Repository:
DOI PREFIX: 10.1029
Date Published:
Journal Name:
Radio Science
Volume:
54
Issue:
11
ISSN:
0048-6604
Page Range / eLocation ID:
p. 1129-1141
Format(s):
Medium: X
Sponsoring Org:
National Science Foundation
More Like this
  1. Abstract Terrestrial Gamma-ray Flashes (TGFs) are intense bursts of gamma rays originating from the Earth’s atmosphere, primarily produced by lightning flashes through relativistic runaway electron avalanches. Observations from the Telescope Array in Utah, equipped with a variety of lightning detection instruments, have revealed detailed insights into TGF initiation and propagation, including their optical emissions. High-speed video cameras and spectroscopic systems have captured optical emissions linked to TGFs, revealing key insights into their initiation and propagation. These findings enhance our understanding of the complex processes underlying TGFs and lightning flashes during thunderstorms. 
    more » « less
  2. Abstract The origin of electrical activity accompanying volcanic ash plumes is an area of heightened interest in volcanology. However, it is unclear how intense an eruption needs to be to produce lightning flashes as opposed to “vent discharges,” which represent the smallest scale of electrical activity. This study targets 97 carefully monitored plumes <3 km high from Sakurajima volcano in Japan, from June 1 to 7, 2015. We use multiparametric measurements from sensors including a nine‐station lightning mapping array and an infrared camera to characterize plume ascent. Findings demonstrate that the impulsive, high velocity plumes (>55 m/s) were most likely to create vent discharges, whereas lightning flashes occurred in plumes with high volume flux. We identified conditions where volcanic lightning occurred without detectable vent discharges, highlighting their independent source mechanisms. Our results imply that plume dynamics govern the charging for volcanic lightning, while the characteristics of the source explosion control vent discharges. 
    more » « less
  3. The lightning-generated whistlers play an important role in the physics of the radiation belts. Magnetospherically reflected (MR) and recently identified specularly reflected (SR) whistlers are the principal contributors to the lightning energy reaching the plasmasphere (Sonwalkar and Reddy, Science Advances, 2024 in press; Sonwalkar and Reddy, AGU 2024). Using plasma wave data from Van Allen Probes and lightning data from the World Wide Lightning Location Network (WWLLN), we performed a correlative study of 22 cases of SR whistlers accompanied by MR whistlers observed in the plasmasphere and the associated causative lightning flashes observed on the ground. Our results can be summarized as follows: (1) The whistlers were observed for 2 < L < 2.5 and 10°S < λm <15°N. (2) Causative lightning flash locations were between 500 and 5000 km of the satellite geomagnetic footprint. (3) Ray tracing analysis in a typical magnetosphere showed that in most cases, the causative lightning was located within 1500 km of ionospheric lightning energy injection points that generated SR and MR whistlers, though lightning energy injected into the ionosphere as far as 3000-4000 km from the lightning location led to detectable SR and MR whistlers. (4) Most of the lightning flashes were located at 10° < λm < 30°, consistent with the observed latitudinal distribution of lightning that shows the majority of lightning flashes occur at low latitudes (<30°) (Orville and Spencer, Monthly Weather Review, 1979). (5) The typical lightning flash energy that generated SR and MR whistlers ranged between 250 J and 6000 J. A whistler propagation model that takes into account lightning location and intensity and various propagation losses could explain the observed intensities of SR and MR whistlers. Our results imply that combining ground-based observations of global lightning activity with the whistler propagation model should provide the levels of lightning-generated whistler mode waves in the plasmasphere, leading to a powerful new space weather technique to monitor lightning-generated plasmaspheric whistler mode waves from the ground. 
    more » « less
  4. Abstract Many of the details of how terrestrial gamma‐ray flashes (TGFs) are produced, including their association with upward‐propagating in‐cloud lightning leader channels, remain poorly understood. Measurements of the low‐frequency radio emissions associated with TGF production continue to provide unique views and key insights into the electrodynamics of this process. Here we report further details on the connection between energetic in‐cloud pulses (EIPs) and TGFs. With coordinated measurements from both ground‐based radio sensors and space‐based gamma‐ray detectors on the Fermi and Reuven Ramaty High Energy Solar Spectroscopic Imager spacecraft, we find that all ten +EIPs that occurred within the searched space‐and‐time window are associated with simultaneous TGFs, including two new TGFs that were not previously identified by the gamma‐ray measurements alone. The results in this study not only solidify the tight connection between +EIPs and TGFs, but also demonstrate the practicability of detecting a subpopulation of TGFs with ground‐based radio sensors alone. 
    more » « less
  5. Abstract The lowest region of the ionosphere, theDregion, plays an important role in magnetosphere‐ionosphere coupling but is challenging to directly observe. The group velocity of the extremely low frequency (ELF; 3–300 Hz) portion of lightning induced electromagnetic radiation can be used to diagnose theDregion electron density profile. Day‐night conditions can be assessed using ELF receivers and lightning detection networks. Analytical formulations and the Long Wave Propagation Capability software package show that ELF group velocity has particular sensitivity to the sharpness of the exponential electron density profile. Applying the technique to sudden ionospheric disturbances shows that the group velocity increases in response to incidence of solar X‐ray flux . A small number of ELF receivers can provide a large‐scale diagnostic of theDregion. ELF remote sensing using lightning is complementary to very low frequency remote sensing and can be used to assess the Earth‐ionosphere propagation channel for very low frequency transmitters. 
    more » « less