Two-Dimensional Structure of Flow Channels and Associated Upward Field-Aligned Currents: Model and Observations

Flow bursts are a major component of transport within the plasma sheet and auroral oval (where they are referred to as flow channels), and lead to a variety of geomagnetic disturbances as they approach the inner plasma sheet (equatorward portion of the auroral oval). However, their two-dimensional s...

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Main Authors: Larry. R. Lyons, Yukitoshi Nishimura, Chih-Ping Wang, Jiang Liu, William. A. Bristow
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-08-01
Series:Frontiers in Astronomy and Space Sciences
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fspas.2021.737946/full
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spelling doaj-9fc1d2d8610d4553b9370d33f820d6b22021-09-03T19:53:35ZengFrontiers Media S.A.Frontiers in Astronomy and Space Sciences2296-987X2021-08-01810.3389/fspas.2021.737946737946Two-Dimensional Structure of Flow Channels and Associated Upward Field-Aligned Currents: Model and ObservationsLarry. R. Lyons0Yukitoshi Nishimura1Chih-Ping Wang2Jiang Liu3Jiang Liu4William. A. Bristow5Department of Atmospheric and Oceanic Sciences, University of California Los Angeles, Los Angeles, CA, United StatesCenter for Space Physics and Department of Electrical and Computer Engineering, Boston University, Boston, MA, United StatesDepartment of Atmospheric and Oceanic Sciences, University of California Los Angeles, Los Angeles, CA, United StatesDepartment of Atmospheric and Oceanic Sciences, University of California Los Angeles, Los Angeles, CA, United StatesDepartment of Earth, Planetary, and Space Sciences, University of California Los Angeles, Los Angeles, CA, United StatesDepartment of Meteorology and Atmospheric Science, 621 Walker Building, The Pennsylvania State University, State College, PA, United StatesFlow bursts are a major component of transport within the plasma sheet and auroral oval (where they are referred to as flow channels), and lead to a variety of geomagnetic disturbances as they approach the inner plasma sheet (equatorward portion of the auroral oval). However, their two-dimensional structure as they approach the inner plasma sheet has received only limited attention. We have examined this structure using both the Rice Convection Model (RCM) and ground-based radar and all sky imager observations. As a result of the energy dependent magnetic drift, the low entropy plasma of a flow burst spreads azimuthally within the inner plasma sheet yielding specific predictions of subauroral polarization stream (SAPS) and dawnside auroral polarization stream (DAPS) enhancements that are related to the field-aligned currents associated with the flow channel. Flow channels approximately centered between the dawn and dusk large-scale convection cells are predicted to give significant enhancements of both SAPS and DAPS, whereas flow channel further toward the dusk (dawn) convection cell show a far more significant enhancement of SAPS (DAPS) than for DAPS (SAPS). We present observations for cases having good coverage of flow channels as they approach the equatorward portion of the auroral oval and find very good qualitative agreement with the above RCM predictions, including the predicted differences with respect to flow burst location. Despite there being an infinite variety of flow channels’ plasma parameters and of background plasma sheet and auroral oval conditions, the observations show the general trends predicted by the RCM simulations with the idealized parameters. This supports that RCM predictions of the azimuthal spread of a low-entropy plasma sheet plasma and its associated FAC and flow responses give a realistic physical description of the structure of plasma sheet flow bursts (auroral oval flow channels) as they reach the inner plasma sheet (near the equatorward edge of the auroral oval).https://www.frontiersin.org/articles/10.3389/fspas.2021.737946/fullflow channelsflow burstssapsdawnside polarization streamconvectionaurora
collection DOAJ
language English
format Article
sources DOAJ
author Larry. R. Lyons
Yukitoshi Nishimura
Chih-Ping Wang
Jiang Liu
Jiang Liu
William. A. Bristow
spellingShingle Larry. R. Lyons
Yukitoshi Nishimura
Chih-Ping Wang
Jiang Liu
Jiang Liu
William. A. Bristow
Two-Dimensional Structure of Flow Channels and Associated Upward Field-Aligned Currents: Model and Observations
Frontiers in Astronomy and Space Sciences
flow channels
flow bursts
saps
dawnside polarization stream
convection
aurora
author_facet Larry. R. Lyons
Yukitoshi Nishimura
Chih-Ping Wang
Jiang Liu
Jiang Liu
William. A. Bristow
author_sort Larry. R. Lyons
title Two-Dimensional Structure of Flow Channels and Associated Upward Field-Aligned Currents: Model and Observations
title_short Two-Dimensional Structure of Flow Channels and Associated Upward Field-Aligned Currents: Model and Observations
title_full Two-Dimensional Structure of Flow Channels and Associated Upward Field-Aligned Currents: Model and Observations
title_fullStr Two-Dimensional Structure of Flow Channels and Associated Upward Field-Aligned Currents: Model and Observations
title_full_unstemmed Two-Dimensional Structure of Flow Channels and Associated Upward Field-Aligned Currents: Model and Observations
title_sort two-dimensional structure of flow channels and associated upward field-aligned currents: model and observations
publisher Frontiers Media S.A.
series Frontiers in Astronomy and Space Sciences
issn 2296-987X
publishDate 2021-08-01
description Flow bursts are a major component of transport within the plasma sheet and auroral oval (where they are referred to as flow channels), and lead to a variety of geomagnetic disturbances as they approach the inner plasma sheet (equatorward portion of the auroral oval). However, their two-dimensional structure as they approach the inner plasma sheet has received only limited attention. We have examined this structure using both the Rice Convection Model (RCM) and ground-based radar and all sky imager observations. As a result of the energy dependent magnetic drift, the low entropy plasma of a flow burst spreads azimuthally within the inner plasma sheet yielding specific predictions of subauroral polarization stream (SAPS) and dawnside auroral polarization stream (DAPS) enhancements that are related to the field-aligned currents associated with the flow channel. Flow channels approximately centered between the dawn and dusk large-scale convection cells are predicted to give significant enhancements of both SAPS and DAPS, whereas flow channel further toward the dusk (dawn) convection cell show a far more significant enhancement of SAPS (DAPS) than for DAPS (SAPS). We present observations for cases having good coverage of flow channels as they approach the equatorward portion of the auroral oval and find very good qualitative agreement with the above RCM predictions, including the predicted differences with respect to flow burst location. Despite there being an infinite variety of flow channels’ plasma parameters and of background plasma sheet and auroral oval conditions, the observations show the general trends predicted by the RCM simulations with the idealized parameters. This supports that RCM predictions of the azimuthal spread of a low-entropy plasma sheet plasma and its associated FAC and flow responses give a realistic physical description of the structure of plasma sheet flow bursts (auroral oval flow channels) as they reach the inner plasma sheet (near the equatorward edge of the auroral oval).
topic flow channels
flow bursts
saps
dawnside polarization stream
convection
aurora
url https://www.frontiersin.org/articles/10.3389/fspas.2021.737946/full
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