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Bibliographic Details
Main Authors: Waszewski, A., Morgan, J. S., Ekers, R., Johnston-Hollitt, M., Cheung, M. C. M., Bhat, N. D. R., Chhetri, R., Fu, S. C.
Format: Preprint
Published: 2025
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Online Access:https://arxiv.org/abs/2506.14155
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author Waszewski, A.
Morgan, J. S.
Ekers, R.
Johnston-Hollitt, M.
Cheung, M. C. M.
Bhat, N. D. R.
Chhetri, R.
Fu, S. C.
author_facet Waszewski, A.
Morgan, J. S.
Ekers, R.
Johnston-Hollitt, M.
Cheung, M. C. M.
Bhat, N. D. R.
Chhetri, R.
Fu, S. C.
contents We present a study of the solar wind over different periods of the solar cycle, specifically focussing on the minimum between solar cycles 24 and 25, and the active, ascending phase of solar cycle 25. With the use of interplanetary scintillation (IPS) data taken by the Murchison Widefield Array (MWA) from mid-2019 and early 2023, we have sampled over a wide range of solar latitudes and elongations, probing a large section of the surrounding heliosphere from $\sim$90 to 140R$_\odot$. The MWA observations provide the highest density of sampled IPS radio sources to date, allowing for an investigation into the latitudinal dependence of the scattering effect caused by the solar wind on a radio source as observed throughout the solar cycle. We find our measurements during periods of heightened solar activity are consistent with a spherically symmetric solar wind. On the other hand, with a reduction in solar activity we find the solar wind density inherits a latitudinal dependence. As is consistent with prior studies, an elliptical function better represents the transition from poles to equator, although we find a more exaggerated sigmoid shaped curve is required to represent the low- to mid-latitude transition region during the minimum of solar cycle 24. We find for a heliospheric distance range of 108 - 123R$_{\odot}$ the reduction ratio between the equator and the southern pole is 1.62$\pm$0.02.
format Preprint
id arxiv_https___arxiv_org_abs_2506_14155
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Latitudinal dependence of the solar wind during periods of high and low activity through interplanetary scintillation
Waszewski, A.
Morgan, J. S.
Ekers, R.
Johnston-Hollitt, M.
Cheung, M. C. M.
Bhat, N. D. R.
Chhetri, R.
Fu, S. C.
Solar and Stellar Astrophysics
We present a study of the solar wind over different periods of the solar cycle, specifically focussing on the minimum between solar cycles 24 and 25, and the active, ascending phase of solar cycle 25. With the use of interplanetary scintillation (IPS) data taken by the Murchison Widefield Array (MWA) from mid-2019 and early 2023, we have sampled over a wide range of solar latitudes and elongations, probing a large section of the surrounding heliosphere from $\sim$90 to 140R$_\odot$. The MWA observations provide the highest density of sampled IPS radio sources to date, allowing for an investigation into the latitudinal dependence of the scattering effect caused by the solar wind on a radio source as observed throughout the solar cycle. We find our measurements during periods of heightened solar activity are consistent with a spherically symmetric solar wind. On the other hand, with a reduction in solar activity we find the solar wind density inherits a latitudinal dependence. As is consistent with prior studies, an elliptical function better represents the transition from poles to equator, although we find a more exaggerated sigmoid shaped curve is required to represent the low- to mid-latitude transition region during the minimum of solar cycle 24. We find for a heliospheric distance range of 108 - 123R$_{\odot}$ the reduction ratio between the equator and the southern pole is 1.62$\pm$0.02.
title Latitudinal dependence of the solar wind during periods of high and low activity through interplanetary scintillation
topic Solar and Stellar Astrophysics
url https://arxiv.org/abs/2506.14155