Prediction of Proton Pressure in the Outer Part of the Inner Magnetosphere Using Machine Learning

Author:

Li S. Y.1234,Kronberg E. A.4ORCID,Mouikis C. G.5ORCID,Luo H.123ORCID,Ge Y. S.123ORCID,Du A. M.123ORCID

Affiliation:

1. CAS Engineering Laboratory for Deep Resources Equipment and Technology Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

2. Innovation Academy for Earth Science CAS Beijing China

3. College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing China

4. Department of Earth and Environmental Sciences (Geophysics) Ludwig‐Maximilians‐Universität München (LMU) Munich Munich Germany

5. Department of Physics and Space Science Center University of New Hampshire NH Durham USA

Abstract

AbstractThe information on plasma pressure in the outer part of the inner magnetosphere is important for simulations of the inner magnetosphere and a better understanding of its dynamics. Based on 17‐year observations from both Cluster Ion Spectrometry and Research with Adaptive Particle Imaging Detector instruments onboard the Cluster mission, we used machine‐learning‐based models to predict proton plasma pressure at energies from ∼40 eV to 4 MeV in the outer part of the inner magnetosphere ( = 5–9). Proton pressure distributions are assumed to be isotropic. The location in the magnetosphere, the property of stably trapped particles, and parameters of solar, solar wind, and geomagnetic activity from the OMNI database are used as predictors. We trained several different machine‐learning‐based models and compared their performances with observations. The results demonstrate that the Extra‐Trees Regressor has the best predicting performance. The Spearman correlation between the observations and predictions by the model is about 70%. The most important parameter for predicting proton pressure in our model is the value, which relates to the property of stably trapped particles. The most important predictor of solar and geomagnetic activity is F10.7 index. Based on the observations and predictions by our model, we find that no matter under quiet or disturbed geomagnetic conditions, both the dusk‐dawn asymmetry at the dayside with higher pressure at the duskside and the day‐night asymmetry with higher pressure at the nightside occur. Our results have direct practical applications, for instance, inputs for simulations of the inner magnetosphere or the reconstruction of the 3‐D magnetospheric electric current system based on the magnetostatic equilibrium.

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science

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