When Plasma Streams Tie up Equatorial Plasma Irregularities with Auroral Ones

Abstract We present a new pattern of storm‐induced ionospheric irregularities behavior at midlatitudes—poleward‐streaming plasma density depletions. Under disturbed conditions, they appear at North America low latitudes as a part of extended postsunset equatorial plasma bubbles, and further, they ar...

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Main Authors: Irina Zakharenkova, Iurii Cherniak
Format: Article
Language:English
Published: Wiley 2020-02-01
Series:Space Weather
Subjects:
Online Access:https://doi.org/10.1029/2019SW002375
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author Irina Zakharenkova
Iurii Cherniak
author_facet Irina Zakharenkova
Iurii Cherniak
author_sort Irina Zakharenkova
collection DOAJ
description Abstract We present a new pattern of storm‐induced ionospheric irregularities behavior at midlatitudes—poleward‐streaming plasma density depletions. Under disturbed conditions, they appear at North America low latitudes as a part of extended postsunset equatorial plasma bubbles, and further, they are streaming from low latitudes in a northwestward, poleward direction toward the main ionospheric trough and auroral irregularities zone. The poleward‐streaming plasma depletions represent a new phenomenon with the similar northwestward transportation path across the continental United States as storm‐enhanced density (SED) plumes. The channels of poleward‐streaming plasma depletions were stretched from low‐latitude base toward higher latitudes—they are found to occur for geomagnetic storms under specific combination of steady southward interplanetary magnetic field, subauroral polarization streams (SAPS) electric fields, and enhanced westward drifts at midlatitudes, resulting in northwestward plasma transportation equatorward of the SAPS region. The poleward‐streaming plasma depletions form an illusion of traveling ionospheric disturbances (TIDs) moving in a poleward, northwestward direction—this propagation direction is opposite to typical equatorward propagation of storm‐induced large‐scale TIDs generated in the auroral zone and propagated toward the equator. This phenomenon is accompanied by strong ionospheric irregularities that occurred over both edges of plasma depletion channel at midlatitudes. For two comparable geomagnetic storms, these poleward‐streaming plasma depletions persisted for several hours, posing a localized threat for GPS‐based positioning applications. Even moderate‐to‐intense storms (Dst minimum−145 nT) can promote such effects at midlatitudes.
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spelling doaj-art-41b25d671f94494b91f48ab16cdcf63d2025-01-14T16:30:20ZengWileySpace Weather1542-73902020-02-01182n/an/a10.1029/2019SW002375When Plasma Streams Tie up Equatorial Plasma Irregularities with Auroral OnesIrina Zakharenkova0Iurii Cherniak1COSMIC Program Office University Corporation for Atmospheric Research Boulder CO USACOSMIC Program Office University Corporation for Atmospheric Research Boulder CO USAAbstract We present a new pattern of storm‐induced ionospheric irregularities behavior at midlatitudes—poleward‐streaming plasma density depletions. Under disturbed conditions, they appear at North America low latitudes as a part of extended postsunset equatorial plasma bubbles, and further, they are streaming from low latitudes in a northwestward, poleward direction toward the main ionospheric trough and auroral irregularities zone. The poleward‐streaming plasma depletions represent a new phenomenon with the similar northwestward transportation path across the continental United States as storm‐enhanced density (SED) plumes. The channels of poleward‐streaming plasma depletions were stretched from low‐latitude base toward higher latitudes—they are found to occur for geomagnetic storms under specific combination of steady southward interplanetary magnetic field, subauroral polarization streams (SAPS) electric fields, and enhanced westward drifts at midlatitudes, resulting in northwestward plasma transportation equatorward of the SAPS region. The poleward‐streaming plasma depletions form an illusion of traveling ionospheric disturbances (TIDs) moving in a poleward, northwestward direction—this propagation direction is opposite to typical equatorward propagation of storm‐induced large‐scale TIDs generated in the auroral zone and propagated toward the equator. This phenomenon is accompanied by strong ionospheric irregularities that occurred over both edges of plasma depletion channel at midlatitudes. For two comparable geomagnetic storms, these poleward‐streaming plasma depletions persisted for several hours, posing a localized threat for GPS‐based positioning applications. Even moderate‐to‐intense storms (Dst minimum−145 nT) can promote such effects at midlatitudes.https://doi.org/10.1029/2019SW002375ionospheric irregularitiesgeomagnetic stormtraveling ionospheric disturbancesequatorial plasma bubblespoleward‐streaming plasma depletions
spellingShingle Irina Zakharenkova
Iurii Cherniak
When Plasma Streams Tie up Equatorial Plasma Irregularities with Auroral Ones
Space Weather
ionospheric irregularities
geomagnetic storm
traveling ionospheric disturbances
equatorial plasma bubbles
poleward‐streaming plasma depletions
title When Plasma Streams Tie up Equatorial Plasma Irregularities with Auroral Ones
title_full When Plasma Streams Tie up Equatorial Plasma Irregularities with Auroral Ones
title_fullStr When Plasma Streams Tie up Equatorial Plasma Irregularities with Auroral Ones
title_full_unstemmed When Plasma Streams Tie up Equatorial Plasma Irregularities with Auroral Ones
title_short When Plasma Streams Tie up Equatorial Plasma Irregularities with Auroral Ones
title_sort when plasma streams tie up equatorial plasma irregularities with auroral ones
topic ionospheric irregularities
geomagnetic storm
traveling ionospheric disturbances
equatorial plasma bubbles
poleward‐streaming plasma depletions
url https://doi.org/10.1029/2019SW002375
work_keys_str_mv AT irinazakharenkova whenplasmastreamstieupequatorialplasmairregularitieswithauroralones
AT iuriicherniak whenplasmastreamstieupequatorialplasmairregularitieswithauroralones