2022
DOI: 10.1029/2022gl098031
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Explicit IMF By‐Dependence of Energetic Protons and the Ring Current

Abstract: The interaction between solar wind, interplanetary magnetic field (IMF) and the Earth's magnetic field is dominated by the north-south (B z ) component of IMF, which is the most important driver of dayside reconnection (Dungey, 1961), and thus the energy input into the magnetosphere. The dawn-dusk (B y ) component of IMF is also known play an important role, leading, for example, to a B y -dependence of the ionospheric convection patterns (

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Cited by 6 publications
(5 citation statements)
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“…The symmetry of the FACs across the noon-night meridional plane breaks in the ionosphere for dawn–dusk IMFs, unlike those cases in which the IMF is purely northward or southward. Using satellite observations and a global MHD model coupled with a ring current model, Holappa et al 29 found that in the northern hemisphere, the flux of energetic magnetospheric protons and the growth rate of the circulation are larger for IMF 0 than for IMF 0. The above studies show that the magnetospheric structure and magnetic reconnection are affected by the IMF component, and the energy transfer characteristics across the magnetopause are also impacted.…”
Section: Introductionmentioning
confidence: 99%
“…The symmetry of the FACs across the noon-night meridional plane breaks in the ionosphere for dawn–dusk IMFs, unlike those cases in which the IMF is purely northward or southward. Using satellite observations and a global MHD model coupled with a ring current model, Holappa et al 29 found that in the northern hemisphere, the flux of energetic magnetospheric protons and the growth rate of the circulation are larger for IMF 0 than for IMF 0. The above studies show that the magnetospheric structure and magnetic reconnection are affected by the IMF component, and the energy transfer characteristics across the magnetopause are also impacted.…”
Section: Introductionmentioning
confidence: 99%
“…(2021b) noted that this By sign dependence is very strong in the winter hemisphere, but it is weak in the summer hemisphere, and is much stronger in the westward electrojet than in the eastward electrojet. Holappa and Buzulokova (2022) noted that the physical mechanisms of IMF By effects, which apply not only to auroral zone electron precipitation and ionospheric conductance but also to the fluxes of energetic magnetosphere protons and the growth rate of the ring current, are still not fully understood.…”
Section: Discussionmentioning
confidence: 99%
“…(2020) analyzed the electron flux data in three different MLT bins, each spanning 8 hr: 20–04 MLT (night), 04–12 MLT (dawn), and 12–20 MLT (dusk) in order to study potential MLT dependence of electron flux on IMF B y effect. Additionally, Holappa and Buzulukova (2022) studied the IMF B y effect on the energetic proton flux specifically in the dusk sector, focusing on the 12 to 24 MLT interval. In this work, the MLT of peak PEJ is used to define the events, following previous works (e.g., Wang & Lühr, 2023, 2024).…”
Section: Data and Processing Methodsmentioning
confidence: 99%