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Imbalanced Regressive Neural Network Model for Whistler-Mode Hiss Waves: Spatial and Temporal Evolution

Journal of Geophysical Research: Space Physics, ISSN: 2169-9402, Vol: 129, Issue: 8
2024
  • 1
    Citations
  • 0
    Usage
  • 4
    Captures
  • 1
    Mentions
  • 0
    Social Media
Metric Options:   Counts1 Year3 Year

Metrics Details

  • Citations
    1
    • Citation Indexes
      1
  • Captures
    4
  • Mentions
    1
    • News Mentions
      1
      • 1

Most Recent News

Reports from University of Colorado Provide New Insights into Networks (Imbalanced Regressive Neural Network Model for Whistler-mode Hiss Waves: Spatial and Temporal Evolution)

2024 SEP 04 (NewsRx) -- By a News Reporter-Staff News Editor at Network Daily News -- A new study on Networks is now available. According

Article Description

Whistler-mode hiss waves are crucial to the dynamics of Earth's radiation belts, particularly in the scattering and loss of energetic electrons and forming the slot region between the inner and outer belts. The generation of hiss waves involves multiple potential mechanisms, which are under active research. Understanding the role of hiss waves in radiation belt dynamics and their generation mechanisms requires analyzing their temporal and spatial evolutions, especially for strong hiss waves. Therefore, we developed an Imbalanced Regressive Neural Network (IR-NN) model for predicting hiss amplitudes. This model addresses the challenge posed by the data imbalance of the hiss data set, which consists of predominantly quiet-time background samples and fewer but significant active-time intense hiss samples. Notably, the IR-NN hiss model excels in predicting strong hiss waves (>100 pT). We investigate the temporal and spatial evolution of hiss wave during a geomagnetic storm on 24–27 October 2017. We show that hiss waves occur within the nominal plasmapause, and follow its dynamically evolving shape. They exhibit intensifications with 1 and 2 hr timescale similar to substorms but with a noticeable time delay. The intensifications begin near dawn and progress toward noon and afternoon. During the storm recovery phase, hiss intensifications may occur in the plume. Additionally, we observe no significant latitudinal dependence of the hiss waves within |MLAT| < 20°. In addition to describing the spatiotemporal evolution of hiss waves, this study highlights the importance of imbalanced regressive methods, given the prevalence of imbalanced data sets in space physics and other real-world applications.

Bibliographic Details

Xiangning Chu; David Malaspina; Jacob Bortnik; Qianli Ma; Donglai Ma; Xiao Chen Shen; Wen Li; Sheng Huang; David P. Hartley

American Geophysical Union (AGU)

Earth and Planetary Sciences

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