Investigation of Ionospheric Small-Scale Plasma Structures associated with Particle Precipitation

We investigate the role of auroral particle precipitation in small-scale (below hundreds of meters) plasma structuring in the auroral ionosphere over the Arctic. To the scope, we together analyse data recorded by an Ionospheric Scintillation Monitor Receiver (ISMR) of Global Navigation Satellite Sys...

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Main Authors: Enengl, Florine, Spogli, Luca, Kotova, Daria, Jin, Yaqi, Oksavik, Kjellmar, Partamies, Noora, Miloch, Wojciech Jacek
Format: Other/Unknown Material
Language:unknown
Published: Authorea, Inc. 2023
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Online Access:http://dx.doi.org/10.22541/essoar.168748399.90008606/v1
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spelling crwinnower:10.22541/essoar.168748399.90008606/v1 2024-06-02T08:02:35+00:00 Investigation of Ionospheric Small-Scale Plasma Structures associated with Particle Precipitation Enengl, Florine Spogli, Luca Kotova, Daria Jin, Yaqi Oksavik, Kjellmar Partamies, Noora Miloch, Wojciech Jacek 2023 http://dx.doi.org/10.22541/essoar.168748399.90008606/v1 unknown Authorea, Inc. posted-content 2023 crwinnower https://doi.org/10.22541/essoar.168748399.90008606/v1 2024-05-07T14:19:23Z We investigate the role of auroral particle precipitation in small-scale (below hundreds of meters) plasma structuring in the auroral ionosphere over the Arctic. To the scope, we together analyse data recorded by an Ionospheric Scintillation Monitor Receiver (ISMR) of Global Navigation Satellite System (GNSS) signals and by an All-Sky Camera located in Longyearbyen, Svalbard (Norway). We leverage on the raw GNSS samples provided at 50 Hz by the ISMR to evaluate amplitude and phase scintillation indices at 1 s time resolution and the Ionosphere-Free Linear Combination at 20 ms time resolution. The simultaneous use of the 1 s GNSS-based scintillation indices allows identifying the scale size of the irregularities involved in plasma structuring in the range of small (up to few hundreds of meters) and medium-scale size ranges (up to few kilometers) for GNSS frequencies and observational geometry. Additionally, they allow identifying the diffractive and refractive nature of the found fluctuations on the recorded GNSS signals. Six strong auroral events and their effects on plasma structuring are studied. Plasma structuring down to scales of hundreds of meters are seen when strong gradients in auroral emissions at 557.7 nm cross the line of sight between the GNSS satellite and receiver. Local magnetic field measurements confirm small-scale structuring processes coinciding with intensification of ionospheric currents. Since 557.7 nm emissions primarily originate from the ionospheric E-region, plasma instabilities from particle precipitation at E-region altitudes are considered to be responsible for the signatures of small-scale plasma structuring highlighted in the GNSS scintillation data. Other/Unknown Material Arctic Longyearbyen Svalbard The Winnower Arctic Longyearbyen Norway Svalbard
institution Open Polar
collection The Winnower
op_collection_id crwinnower
language unknown
description We investigate the role of auroral particle precipitation in small-scale (below hundreds of meters) plasma structuring in the auroral ionosphere over the Arctic. To the scope, we together analyse data recorded by an Ionospheric Scintillation Monitor Receiver (ISMR) of Global Navigation Satellite System (GNSS) signals and by an All-Sky Camera located in Longyearbyen, Svalbard (Norway). We leverage on the raw GNSS samples provided at 50 Hz by the ISMR to evaluate amplitude and phase scintillation indices at 1 s time resolution and the Ionosphere-Free Linear Combination at 20 ms time resolution. The simultaneous use of the 1 s GNSS-based scintillation indices allows identifying the scale size of the irregularities involved in plasma structuring in the range of small (up to few hundreds of meters) and medium-scale size ranges (up to few kilometers) for GNSS frequencies and observational geometry. Additionally, they allow identifying the diffractive and refractive nature of the found fluctuations on the recorded GNSS signals. Six strong auroral events and their effects on plasma structuring are studied. Plasma structuring down to scales of hundreds of meters are seen when strong gradients in auroral emissions at 557.7 nm cross the line of sight between the GNSS satellite and receiver. Local magnetic field measurements confirm small-scale structuring processes coinciding with intensification of ionospheric currents. Since 557.7 nm emissions primarily originate from the ionospheric E-region, plasma instabilities from particle precipitation at E-region altitudes are considered to be responsible for the signatures of small-scale plasma structuring highlighted in the GNSS scintillation data.
format Other/Unknown Material
author Enengl, Florine
Spogli, Luca
Kotova, Daria
Jin, Yaqi
Oksavik, Kjellmar
Partamies, Noora
Miloch, Wojciech Jacek
spellingShingle Enengl, Florine
Spogli, Luca
Kotova, Daria
Jin, Yaqi
Oksavik, Kjellmar
Partamies, Noora
Miloch, Wojciech Jacek
Investigation of Ionospheric Small-Scale Plasma Structures associated with Particle Precipitation
author_facet Enengl, Florine
Spogli, Luca
Kotova, Daria
Jin, Yaqi
Oksavik, Kjellmar
Partamies, Noora
Miloch, Wojciech Jacek
author_sort Enengl, Florine
title Investigation of Ionospheric Small-Scale Plasma Structures associated with Particle Precipitation
title_short Investigation of Ionospheric Small-Scale Plasma Structures associated with Particle Precipitation
title_full Investigation of Ionospheric Small-Scale Plasma Structures associated with Particle Precipitation
title_fullStr Investigation of Ionospheric Small-Scale Plasma Structures associated with Particle Precipitation
title_full_unstemmed Investigation of Ionospheric Small-Scale Plasma Structures associated with Particle Precipitation
title_sort investigation of ionospheric small-scale plasma structures associated with particle precipitation
publisher Authorea, Inc.
publishDate 2023
url http://dx.doi.org/10.22541/essoar.168748399.90008606/v1
geographic Arctic
Longyearbyen
Norway
Svalbard
geographic_facet Arctic
Longyearbyen
Norway
Svalbard
genre Arctic
Longyearbyen
Svalbard
genre_facet Arctic
Longyearbyen
Svalbard
op_doi https://doi.org/10.22541/essoar.168748399.90008606/v1
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