(Un)Explained EMIC Waves: Understanding Quiet Time EMIC Wave Drivers

Abstract Electromagnetic ion cyclotron (EMIC) waves are known to be generated through cyclotron resonance with the local ion particle population and grow when there is a large enough temperature anisotropy. In general, these temperature anisotropies necessary for wave growth are found to be associated with either solar wind pressure pulses or particle injections during geomagnetic storms or substorms. However, some EMIC events do not show any clear association with these known drivers and appear unexplained. In our analysis of high‐amplitude (1 nT) non‐storm time EMIC waves, we find that 24 out of the 223 (11%) EMIC events with peak amplitude greater than 1 nT were not found to be associated with any clear EMIC wave driver. This raises a compelling question: What magnetospheric or solar wind driver provides the free energy to grow these quiet‐time EMIC waves? Here, we examine two EMIC events on 13 April 2017 and 13 February 2014, which were excited during extremely quiet solar wind and geomagnetic conditions. An in‐depth analysis of field and particle measurements from multiple data sets, including ground and in situ data for these two events, indicates that extremely weak and otherwise insignificant pressure values and/or very weak substorm injections occurring multiple hours before the event play a significant role in quiet time wave generation.

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Publication Details

Journal
Journal of Geophysical Research Space Physics
Published
2025-08-01
DOI
https://doi.org/10.1029/2024ja033125
Primary Topic
Ionosphere and magnetosphere dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

(Un)Explained EMIC Waves: Understanding Quiet Time EMIC Wave Drivers

B. Remya, Tero Raita, David Gary Sibeck, Alexa Halford et al.
Journal of Geophysical Research Space Physics
Ionosphere and magnetosphere dynamics
article

(Un)Explained EMIC Waves: Understanding Quiet Time EMIC Wave Drivers

B. Remya, Tero Raita, David Gary Sibeck, Alexa Halford, B. Grison, Ashok Priyadarshan Dimri, T. M. Esman, Dedong Wang, D. B. Graham, P. A. Fernandes, S. J. Noh, Julia Himmelsbach
article en

Abstract

Abstract Electromagnetic ion cyclotron (EMIC) waves are known to be generated through cyclotron resonance with the local ion particle population and grow when there is a large enough temperature anisotropy. In general, these temperature anisotropies necessary for wave growth are found to be associated with either solar wind pressure pulses or particle injections during geomagnetic storms or substorms. However, some EMIC events do not show any clear association with these known drivers and appear unexplained. In our analysis of high‐amplitude (1 nT) non‐storm time EMIC waves, we find that 24 out of the 223 (11%) EMIC events with peak amplitude greater than 1 nT were not found to be associated with any clear EMIC wave driver. This raises a compelling question: What magnetospheric or solar wind driver provides the free energy to grow these quiet‐time EMIC waves? Here, we examine two EMIC events on 13 April 2017 and 13 February 2014, which were excited during extremely quiet solar wind and geomagnetic conditions. An in‐depth analysis of field and particle measurements from multiple data sets, including ground and in situ data for these two events, indicates that extremely weak and otherwise insignificant pressure values and/or very weak substorm injections occurring multiple hours before the event play a significant role in quiet time wave generation.

Journal of Geophysical Research Space PhysicsVol. 130(8)
Goddard Space Flight Center (US), Swedish Institute of Space Physics (SE), Los Alamos National Laboratory (US), Czech Academy of Sciences, Institute of Atmospheric Physics (CZ), GFZ Helmholtz Centre for Geosciences (DE), Geological Survey of India (IN), University of Oulu (FI)
Department of Science and Technology, Ministry of Science and Technology, India, Oulun Yliopisto, Indian Institute of Geomagnetism
Affordable and clean energy
Openalex Percentile: Top 85%
Ionosphere and magnetosphere dynamics
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