Classifying Magnetic Reconnection Regions Using <i>k</i>‐Means Clustering: Applications to Energy Partition

Abstract Magnetic reconnection is a fundamental plasma process which facilitates the conversion of magnetic energy to particle energies. This local process both contributes to and is affected by a larger system, being dependent on plasma conditions and transporting energy around the system, such as Earth's magnetosphere. When studying the reconnection process with in situ spacecraft data, it can be difficult to determine where spacecraft are in relation to the reconnection structure. In this work, we use k ‐means clustering, an unsupervised machine learning technique, to identify regions in a 2.5‐D PIC simulation of symmetric magnetic reconnection with conditions comparable to those observed in Earth's magnetotail. This allows energy flux densities to be attributed to these regions. The ion enthalpy flux density is the most dominant form of energy flux density in the outflows, agreeing with previous studies. Poynting flux density may be dominant at some points in the outflows and is only half that of the Poynting flux density in the separatrices. The proportion of outflowing particle energy flux decreases as guide field increases. We find that k ‐means is beneficial for analyzing data and comparing between simulations and in situ data. This demonstrates an approach which may be applied to large volumes of data to determine statistically different regions within phenomena in simulations and could be extended to in situ observations, applicable to future multi‐point missions.

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Publication Details

Journal
Journal of Geophysical Research Space Physics
Published
2024-10-01
DOI
https://doi.org/10.1029/2024ja033010
Citations
2
Primary Topic
Geomagnetism and Paleomagnetism Studies
Type
article
Field-Weighted Citation Impact
0.47

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article

Classifying Magnetic Reconnection Regions Using k‐Means Clustering: Applications to Energy Partition

Cara L. Waters, D. L. Newman, J. P. Eastwood, Naïs Fargette et al.
2 citations
Journal of Geophysical Research Space Physics
Geomagnetism and Paleomagnetism Studies
0.47
article

Classifying Magnetic Reconnection Regions Using k‐Means Clustering: Applications to Energy Partition

Cara L. Waters, D. L. Newman, J. P. Eastwood, Naïs Fargette, M. V. Goldman
article en
2 citations

Abstract

Abstract Magnetic reconnection is a fundamental plasma process which facilitates the conversion of magnetic energy to particle energies. This local process both contributes to and is affected by a larger system, being dependent on plasma conditions and transporting energy around the system, such as Earth's magnetosphere. When studying the reconnection process with in situ spacecraft data, it can be difficult to determine where spacecraft are in relation to the reconnection structure. In this work, we use k ‐means clustering, an unsupervised machine learning technique, to identify regions in a 2.5‐D PIC simulation of symmetric magnetic reconnection with conditions comparable to those observed in Earth's magnetotail. This allows energy flux densities to be attributed to these regions. The ion enthalpy flux density is the most dominant form of energy flux density in the outflows, agreeing with previous studies. Poynting flux density may be dominant at some points in the outflows and is only half that of the Poynting flux density in the separatrices. The proportion of outflowing particle energy flux decreases as guide field increases. We find that k ‐means is beneficial for analyzing data and comparing between simulations and in situ data. This demonstrates an approach which may be applied to large volumes of data to determine statistically different regions within phenomena in simulations and could be extended to in situ observations, applicable to future multi‐point missions.

Journal of Geophysical Research Space PhysicsVol. 129(10)
University of Colorado Boulder (US), Imperial College London (GB)
UK Research and Innovation, Science and Technology Facilities Council
Openalex Percentile: Top 34%
Geomagnetism and Paleomagnetism Studies
0.47
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