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Energization of the Ring Current by Substorms

Journal Article · · Journal of Geophysical Research. Space Physics
DOI:https://doi.org/10.1029/2018JA025766· OSTI ID:1484669
 [1];  [1];  [2];  [1];  [3];  [4];  [5];  [6];  [6]
  1. Univ. College London (United Kingdom). Dept. of Space and Climate Physics. Mullard Space Science Lab.
  2. British Antarctic Survey, Cambridge (United Kingdom)
  3. Johns Hopkins Univ., Baltimore, MD (United States). Applied Physics Lab.
  4. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
  5. Univ. of New Hampshire, Durham, NH (United States). Inst. for the Study of Earth, Oceans, and Space
  6. Univ. of Southampton (United Kingdom). Dept. of Physics and Astronomy
The substorm process releases large amounts of energy into the magnetospheric system, although where the energy is transferred to and how it is partitioned remains an open question. In this study, we address whether the substorm process contributes a significant amount of energy to the ring current. The ring current is a highly variable region, and understanding the energization processes provides valuable insight into how substorm-ring current coupling may contribute to the generation of storm conditions and provide a source of energy for wave driving. In order to quantify the energy input into the ring current during the substorm process, we analyze Radiation Belt Storm Probes Ion Composition Experiment and Helium Oxygen Proton Electron ion flux measurements for H+, O+, and He+. The energy content of the ring current is estimated and binned spatially for L and magnetic local time. The results are combined with an independently derived substorm event list to perform a statistical analysis of variations in the ring current energy content with substorm phase. We show that the ring current energy is significantly higher in the expansion phase compared to the growth phase, with the energy enhancement persisting into the substorm recovery phase. The characteristics of the energy enhancement suggest the injection of energized ions from the tail plasma sheet following substorm onset. The local time variations indicate a loss of energetic H+ ions in the afternoon sector, likely due to wave-particle interactions. Overall, we find that the average energy input into the ring current is ~9% of the previously reported energy released during substorms.
Research Organization:
Los Alamos National Laboratory (LANL)
Sponsoring Organization:
National Aeronautics and Space Administration (NASA) (United States); Natural Environment Research Council (NERC) (United Kingdom); Science and Technology Facilities Council (STFC) (United Kingdom); USDOE
Grant/Contract Number:
89233218CNA000001
OSTI ID:
1484669
Report Number(s):
LA-UR-18-28975
Journal Information:
Journal of Geophysical Research. Space Physics, Journal Name: Journal of Geophysical Research. Space Physics Journal Issue: 10 Vol. 123; ISSN 2169-9380
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English

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Cited By (6)

Variations of Field Line Eigenfrequencies With Ring Current Intensity journal November 2018
The Influence of Substorms on Extreme Rates of Change of the Surface Horizontal Magnetic Field in the United Kingdom journal June 2019
Contribution of Bursty Bulk Flows to the Global Dipolarization of the Magnetotail During an Isolated Substorm journal November 2019
How Do Ultra‐Low Frequency Waves Access the Inner Magnetosphere During Geomagnetic Storms? journal October 2019
Substorm‐Ring Current Coupling: A Comparison of Isolated and Compound Substorms journal August 2019
The Variation of Resonating Magnetospheric Field Lines With Changing Geomagnetic and Solar Wind Conditions journal July 2019

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