Survey of electron density changes in the daytime ionosphere over the Arecibo observatory due to lightning and solar flares

Abstract Optical observations of transient luminous events and remote-sensing of the lower ionosphere with low-frequency radio waves have demonstrated that thunderstorms and lightning can have substantial impacts in the nighttime ionospheric D region. However, it remains a challenge to quantify such...

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Main Authors: Caitano L. da Silva, Sophia D. Salazar, Christiano G. M. Brum, Pedrina Terra
Format: Article
Language:English
Published: Nature Publishing Group 2021-05-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-89662-x
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spelling doaj-6b8c5576dda0403f8ed80e49ea235e652021-05-16T11:23:25ZengNature Publishing GroupScientific Reports2045-23222021-05-0111111210.1038/s41598-021-89662-xSurvey of electron density changes in the daytime ionosphere over the Arecibo observatory due to lightning and solar flaresCaitano L. da Silva0Sophia D. Salazar1Christiano G. M. Brum2Pedrina Terra3Department of Physics and Langmuir Lab, New Mexico TechDepartment of Physics and Langmuir Lab, New Mexico TechArecibo Observatory and University of Central FloridaArecibo Observatory and University of Central FloridaAbstract Optical observations of transient luminous events and remote-sensing of the lower ionosphere with low-frequency radio waves have demonstrated that thunderstorms and lightning can have substantial impacts in the nighttime ionospheric D region. However, it remains a challenge to quantify such effects in the daytime lower ionosphere. The wealth of electron density data acquired over the years by the Arecibo Observatory incoherent scatter radar (ISR) with high vertical spatial resolution (300-m in the present study), combined with its tropical location in a region of high lightning activity, indicate a potentially transformative pathway to address this issue. Through a systematic survey, we show that daytime sudden electron density changes registered by Arecibo’s ISR during thunderstorm times are on average different than the ones happening during fair weather conditions (driven by other external factors). These changes typically correspond to electron density depletions in the D and E region. The survey also shows that these disturbances are different than the ones associated with solar flares, which tend to have longer duration and most often correspond to an increase in the local electron density content.https://doi.org/10.1038/s41598-021-89662-x
collection DOAJ
language English
format Article
sources DOAJ
author Caitano L. da Silva
Sophia D. Salazar
Christiano G. M. Brum
Pedrina Terra
spellingShingle Caitano L. da Silva
Sophia D. Salazar
Christiano G. M. Brum
Pedrina Terra
Survey of electron density changes in the daytime ionosphere over the Arecibo observatory due to lightning and solar flares
Scientific Reports
author_facet Caitano L. da Silva
Sophia D. Salazar
Christiano G. M. Brum
Pedrina Terra
author_sort Caitano L. da Silva
title Survey of electron density changes in the daytime ionosphere over the Arecibo observatory due to lightning and solar flares
title_short Survey of electron density changes in the daytime ionosphere over the Arecibo observatory due to lightning and solar flares
title_full Survey of electron density changes in the daytime ionosphere over the Arecibo observatory due to lightning and solar flares
title_fullStr Survey of electron density changes in the daytime ionosphere over the Arecibo observatory due to lightning and solar flares
title_full_unstemmed Survey of electron density changes in the daytime ionosphere over the Arecibo observatory due to lightning and solar flares
title_sort survey of electron density changes in the daytime ionosphere over the arecibo observatory due to lightning and solar flares
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-05-01
description Abstract Optical observations of transient luminous events and remote-sensing of the lower ionosphere with low-frequency radio waves have demonstrated that thunderstorms and lightning can have substantial impacts in the nighttime ionospheric D region. However, it remains a challenge to quantify such effects in the daytime lower ionosphere. The wealth of electron density data acquired over the years by the Arecibo Observatory incoherent scatter radar (ISR) with high vertical spatial resolution (300-m in the present study), combined with its tropical location in a region of high lightning activity, indicate a potentially transformative pathway to address this issue. Through a systematic survey, we show that daytime sudden electron density changes registered by Arecibo’s ISR during thunderstorm times are on average different than the ones happening during fair weather conditions (driven by other external factors). These changes typically correspond to electron density depletions in the D and E region. The survey also shows that these disturbances are different than the ones associated with solar flares, which tend to have longer duration and most often correspond to an increase in the local electron density content.
url https://doi.org/10.1038/s41598-021-89662-x
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