IMF B y influence on fast earthward convection flows in the near-lunar magnetotail

Abstract This study investigates the effects of non-zero IMF B y on the magnetotail B y and fast earthward ion convection (V ⊥ > 200 km/s, "⊥" indicates perpendicular to the magnetic field) in the near-lunar magnetotail plasma sheet using the plasma parameters and magnetic field detecte...

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Main Authors: T. C. Liu, T. Pitkänen, S. Nilsson, A. Kullen, J.-S. Park, M. Hamrin, W. S. Shang, H. Z. Wang, S. T. Yao
Format: Article
Language:English
Published: SpringerOpen 2025-02-01
Series:Geoscience Letters
Online Access:https://doi.org/10.1186/s40562-025-00379-5
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author T. C. Liu
T. Pitkänen
S. Nilsson
A. Kullen
J.-S. Park
M. Hamrin
W. S. Shang
H. Z. Wang
S. T. Yao
author_facet T. C. Liu
T. Pitkänen
S. Nilsson
A. Kullen
J.-S. Park
M. Hamrin
W. S. Shang
H. Z. Wang
S. T. Yao
author_sort T. C. Liu
collection DOAJ
description Abstract This study investigates the effects of non-zero IMF B y on the magnetotail B y and fast earthward ion convection (V ⊥ > 200 km/s, "⊥" indicates perpendicular to the magnetic field) in the near-lunar magnetotail plasma sheet using the plasma parameters and magnetic field detected by the ARTEMIS (Acceleration, Reconnection, Turbulence, and Electrodynamics of the Moon’s Interaction with the Sun) P1 satellite during the period 2011–2022. We find that the magnetotail B y with in the same direction as IMF B y dominates the entire region. The IMF B y influence is hemisphere-independent, but shows a dusk-dawn asymmetry with the IMF B y effect being weaker in the premidnight region than in the postmidnight region. We also find that the IMF B y influence on earthward fast convection results in an interhemispheric flow asymmetry and it is highly correlated with the direction of magnetotail B y. The statistical results indicate that occasionally localized dynamics can have a significant effect on magnetotail B y and V ⊥.
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series Geoscience Letters
spelling doaj-art-0ffd81fd62ee4144a6ded11b24698c8d2025-02-09T12:40:03ZengSpringerOpenGeoscience Letters2196-40922025-02-0112111010.1186/s40562-025-00379-5IMF B y influence on fast earthward convection flows in the near-lunar magnetotailT. C. Liu0T. Pitkänen1S. Nilsson2A. Kullen3J.-S. Park4M. Hamrin5W. S. Shang6H. Z. Wang7S. T. Yao8Shandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, Institute of Space Sciences, Shandong UniversityShandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, Institute of Space Sciences, Shandong UniversityDepartment of Physics, Umeå UniversitySpace and Plasma Physics, School of Electrical Engineering and Computer Science, Royal Institute of TechnologyShandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, Institute of Space Sciences, Shandong UniversityDepartment of Physics, Umeå UniversityShandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, Institute of Space Sciences, Shandong UniversityShandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, Institute of Space Sciences, Shandong UniversityShandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, Institute of Space Sciences, Shandong UniversityAbstract This study investigates the effects of non-zero IMF B y on the magnetotail B y and fast earthward ion convection (V ⊥ > 200 km/s, "⊥" indicates perpendicular to the magnetic field) in the near-lunar magnetotail plasma sheet using the plasma parameters and magnetic field detected by the ARTEMIS (Acceleration, Reconnection, Turbulence, and Electrodynamics of the Moon’s Interaction with the Sun) P1 satellite during the period 2011–2022. We find that the magnetotail B y with in the same direction as IMF B y dominates the entire region. The IMF B y influence is hemisphere-independent, but shows a dusk-dawn asymmetry with the IMF B y effect being weaker in the premidnight region than in the postmidnight region. We also find that the IMF B y influence on earthward fast convection results in an interhemispheric flow asymmetry and it is highly correlated with the direction of magnetotail B y. The statistical results indicate that occasionally localized dynamics can have a significant effect on magnetotail B y and V ⊥.https://doi.org/10.1186/s40562-025-00379-5
spellingShingle T. C. Liu
T. Pitkänen
S. Nilsson
A. Kullen
J.-S. Park
M. Hamrin
W. S. Shang
H. Z. Wang
S. T. Yao
IMF B y influence on fast earthward convection flows in the near-lunar magnetotail
Geoscience Letters
title IMF B y influence on fast earthward convection flows in the near-lunar magnetotail
title_full IMF B y influence on fast earthward convection flows in the near-lunar magnetotail
title_fullStr IMF B y influence on fast earthward convection flows in the near-lunar magnetotail
title_full_unstemmed IMF B y influence on fast earthward convection flows in the near-lunar magnetotail
title_short IMF B y influence on fast earthward convection flows in the near-lunar magnetotail
title_sort imf b y influence on fast earthward convection flows in the near lunar magnetotail
url https://doi.org/10.1186/s40562-025-00379-5
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