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Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations
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Zeitschriftentitel: | Radio Science |
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Personen und Körperschaften: | , , , |
In: | Radio Science, 53, 2018, 4, S. 472-484 |
Format: | E-Article |
Sprache: | Englisch |
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American Geophysical Union (AGU)
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author_facet |
Chakraborty, S. Ruohoniemi, J. M. Baker, J. B. H. Nishitani, N. Chakraborty, S. Ruohoniemi, J. M. Baker, J. B. H. Nishitani, N. |
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author |
Chakraborty, S. Ruohoniemi, J. M. Baker, J. B. H. Nishitani, N. |
spellingShingle |
Chakraborty, S. Ruohoniemi, J. M. Baker, J. B. H. Nishitani, N. Radio Science Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations Electrical and Electronic Engineering General Earth and Planetary Sciences Condensed Matter Physics |
author_sort |
chakraborty, s. |
spelling |
Chakraborty, S. Ruohoniemi, J. M. Baker, J. B. H. Nishitani, N. 0048-6604 1944-799X American Geophysical Union (AGU) Electrical and Electronic Engineering General Earth and Planetary Sciences Condensed Matter Physics http://dx.doi.org/10.1002/2017rs006488 <jats:title>Abstract</jats:title><jats:p>Short‐wave fadeout (SWF) is a well‐known radio wave anomaly which follows Earth‐directed solar flares and leads to severe disruption of transionospheric high‐frequency systems. The disruption is produced by flare‐enhanced soft and hard X‐rays that penetrate to the <jats:italic>D</jats:italic> layer where they dramatically enhance ionization leading to heavy high‐frequency absorption over much of the dayside for an hour or more. In this paper, we describe how Super Dual Auroral Radar Network (SuperDARN) observations can be exploited to analyze SWF events. Superposed epoch analysis of multiple signatures reveals the typical characteristics of SWF. The number of SuperDARN ground scatter echoes drops suddenly (≈100 s) and sharply after a solar flare, reaching a maximum depth of suppression within a few tens of minutes, and then recovering to pre‐SWF conditions over half an hour or so. The depth of echo suppression depends on the solar zenith angle, radio wave frequency, and intensity of the flare. Furthermore, ground scatter echoes typically exhibit a sudden phase change leading to a dramatic increase in apparent Doppler velocity (the so‐called “Doppler flash”), which statistically precedes the dropout in ground scatter echoes. We report here on the characterization of SWF effects in SuperDARN ground scatter observations produced by several X class solar flares. We also describe the functional dependence of peak Doppler flash on solar zenith angle, frequency, and peak intensity of solar flux.</jats:p> Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations Radio Science |
doi_str_mv |
10.1002/2017rs006488 |
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title |
Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_unstemmed |
Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_full |
Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_fullStr |
Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_full_unstemmed |
Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_short |
Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_sort |
characterization of short‐wave fadeout seen in daytime superdarn ground scatter observations |
topic |
Electrical and Electronic Engineering General Earth and Planetary Sciences Condensed Matter Physics |
url |
http://dx.doi.org/10.1002/2017rs006488 |
publishDate |
2018 |
physical |
472-484 |
description |
<jats:title>Abstract</jats:title><jats:p>Short‐wave fadeout (SWF) is a well‐known radio wave anomaly which follows Earth‐directed solar flares and leads to severe disruption of transionospheric high‐frequency systems. The disruption is produced by flare‐enhanced soft and hard X‐rays that penetrate to the <jats:italic>D</jats:italic> layer where they dramatically enhance ionization leading to heavy high‐frequency absorption over much of the dayside for an hour or more. In this paper, we describe how Super Dual Auroral Radar Network (SuperDARN) observations can be exploited to analyze SWF events. Superposed epoch analysis of multiple signatures reveals the typical characteristics of SWF. The number of SuperDARN ground scatter echoes drops suddenly (≈100 s) and sharply after a solar flare, reaching a maximum depth of suppression within a few tens of minutes, and then recovering to pre‐SWF conditions over half an hour or so. The depth of echo suppression depends on the solar zenith angle, radio wave frequency, and intensity of the flare. Furthermore, ground scatter echoes typically exhibit a sudden phase change leading to a dramatic increase in apparent Doppler velocity (the so‐called “Doppler flash”), which statistically precedes the dropout in ground scatter echoes. We report here on the characterization of SWF effects in SuperDARN ground scatter observations produced by several X class solar flares. We also describe the functional dependence of peak Doppler flash on solar zenith angle, frequency, and peak intensity of solar flux.</jats:p> |
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author | Chakraborty, S., Ruohoniemi, J. M., Baker, J. B. H., Nishitani, N. |
author_facet | Chakraborty, S., Ruohoniemi, J. M., Baker, J. B. H., Nishitani, N., Chakraborty, S., Ruohoniemi, J. M., Baker, J. B. H., Nishitani, N. |
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description | <jats:title>Abstract</jats:title><jats:p>Short‐wave fadeout (SWF) is a well‐known radio wave anomaly which follows Earth‐directed solar flares and leads to severe disruption of transionospheric high‐frequency systems. The disruption is produced by flare‐enhanced soft and hard X‐rays that penetrate to the <jats:italic>D</jats:italic> layer where they dramatically enhance ionization leading to heavy high‐frequency absorption over much of the dayside for an hour or more. In this paper, we describe how Super Dual Auroral Radar Network (SuperDARN) observations can be exploited to analyze SWF events. Superposed epoch analysis of multiple signatures reveals the typical characteristics of SWF. The number of SuperDARN ground scatter echoes drops suddenly (≈100 s) and sharply after a solar flare, reaching a maximum depth of suppression within a few tens of minutes, and then recovering to pre‐SWF conditions over half an hour or so. The depth of echo suppression depends on the solar zenith angle, radio wave frequency, and intensity of the flare. Furthermore, ground scatter echoes typically exhibit a sudden phase change leading to a dramatic increase in apparent Doppler velocity (the so‐called “Doppler flash”), which statistically precedes the dropout in ground scatter echoes. We report here on the characterization of SWF effects in SuperDARN ground scatter observations produced by several X class solar flares. We also describe the functional dependence of peak Doppler flash on solar zenith angle, frequency, and peak intensity of solar flux.</jats:p> |
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spelling | Chakraborty, S. Ruohoniemi, J. M. Baker, J. B. H. Nishitani, N. 0048-6604 1944-799X American Geophysical Union (AGU) Electrical and Electronic Engineering General Earth and Planetary Sciences Condensed Matter Physics http://dx.doi.org/10.1002/2017rs006488 <jats:title>Abstract</jats:title><jats:p>Short‐wave fadeout (SWF) is a well‐known radio wave anomaly which follows Earth‐directed solar flares and leads to severe disruption of transionospheric high‐frequency systems. The disruption is produced by flare‐enhanced soft and hard X‐rays that penetrate to the <jats:italic>D</jats:italic> layer where they dramatically enhance ionization leading to heavy high‐frequency absorption over much of the dayside for an hour or more. In this paper, we describe how Super Dual Auroral Radar Network (SuperDARN) observations can be exploited to analyze SWF events. Superposed epoch analysis of multiple signatures reveals the typical characteristics of SWF. The number of SuperDARN ground scatter echoes drops suddenly (≈100 s) and sharply after a solar flare, reaching a maximum depth of suppression within a few tens of minutes, and then recovering to pre‐SWF conditions over half an hour or so. The depth of echo suppression depends on the solar zenith angle, radio wave frequency, and intensity of the flare. Furthermore, ground scatter echoes typically exhibit a sudden phase change leading to a dramatic increase in apparent Doppler velocity (the so‐called “Doppler flash”), which statistically precedes the dropout in ground scatter echoes. We report here on the characterization of SWF effects in SuperDARN ground scatter observations produced by several X class solar flares. We also describe the functional dependence of peak Doppler flash on solar zenith angle, frequency, and peak intensity of solar flux.</jats:p> Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations Radio Science |
spellingShingle | Chakraborty, S., Ruohoniemi, J. M., Baker, J. B. H., Nishitani, N., Radio Science, Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations, Electrical and Electronic Engineering, General Earth and Planetary Sciences, Condensed Matter Physics |
title | Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_full | Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_fullStr | Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_full_unstemmed | Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_short | Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
title_sort | characterization of short‐wave fadeout seen in daytime superdarn ground scatter observations |
title_unstemmed | Characterization of Short‐Wave Fadeout Seen in Daytime SuperDARN Ground Scatter Observations |
topic | Electrical and Electronic Engineering, General Earth and Planetary Sciences, Condensed Matter Physics |
url | http://dx.doi.org/10.1002/2017rs006488 |