Ultra-low-frequency wave power in the magnetotail lobes 1. Relation to substorm Onsets and the auroral electrojet index

Date

1990-10

Department

Program

Citation of Original Publication

Smith, R. A., M. L. Goldstein, M. R. Sands, R. P. Lepping, C. K. Goertz, B. G. Harrold, C. A. Fitch, and L.-H. Shan. “Ultra-Low-Frequency Wave Power in the Magnetotail Lobes 1. Relation to Substorm Onsets and the Auroral Electrojet Index.” Geophysical Research Letters 17, no. 11 (1990): 1845–48. https://doi.org/10.1029/GL017i011p01845.

Rights

This work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
Public Domain Mark 1.0

Subjects

Abstract

Time series observations of the magnetotail lobe magnetic field have been Fourier analyzed to compute the frequency-weighted energy density Pfz in the range 1–30 mHz. Pfz is generally observed in the range 10⁻⁴ – 10⁻² γ² – Hz, with a mean value of 1.2 × 10⁻³ γ² – Hz during substorm phases and 1.0 × 10⁻³ γ² – Hz in the comparison intervals. No strong correlation of Pfz is found with AE in set of intervals, but during substorm growth phases Pfz may vary by an order of magnitude over time scales of 30 min, with a tendency for higher power levels to occur later in the growth phase. Increases in Pfz are seen to precede by ∼ 10 min localized expansive phase activity observed in individual magnetograms. The observed levels of Pfz during growth phase are in general accord with the requirements of the thermal catastrophe substorm model.