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AGU: Geophysical Research Letters

 

Index Terms

  • Atmospheric Composition and Structure: Middle atmosphere—energy deposition
  • Meteorology and Atmospheric Dynamics: Atmospheric electricity
  • Meteorology and Atmospheric Dynamics: Lightning
  • Meteorology and Atmospheric Dynamics: Middle atmosphere dynamics

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 29, 1462, 4 PP., 2002
doi:10.1029/2001GL014018

Electron energy and electric field estimates in sprites derived from ionized and neutral N2 emissions

J. Morrill

E. O Hulburt Center for Space Research, Naval Research Laboratory, Washington, DC, USA.

E. Bucsela

Goddard Earth Science and Technology Center, Baltimore, MD, USA.

C. Siefring

Plasma Physics Division, Naval Research Laboratory, Washington DC, USA.

M. Heavner

Los Alamos National Laboratory, Los Alamos, NM, USA.

S. Berg

Computational Physics Inc., Springfield, VA, USA.

D. Moudry

Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AL, USA.

S. Slinker

Plasma Physics Division, Naval Research Laboratory, Washington DC, USA.

R. Fernsler

Plasma Physics Division, Naval Research Laboratory, Washington DC, USA.

E. Wescott

Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AL, USA.

D. Sentman

Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AL, USA.

D. Osborne

Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AL, USA.

During the EXL98 aircraft mission, sprites and blue jets were observed by narrow band cameras that measure the N2+ 1NG (0,1) band at 4278Å and the N2 2PG (0,0) band at 3370Å. We discuss the observations (∼1km resolution), instrumental and atmospheric corrections, and altitude profiles of ionized (1NG) and neutral (2PG) emission observed during a specific sprite. The ratio of ionized-to-neutral emission indicates a relative enhancement of ion emission below 55km. Characteristic electron energies (ECh) and electric fields (E) are derived from these emission ratios using excitation rates computed from a model that solves the Boltzmann equation as a function of electric field. Up to 55km E follows the breakdown field (Ek) and ECh is ∼2.2eV. Above 55km E drops below Ek and ECh drops to ∼1.75eV near 60km.

Published 28 May 2002.

Citation: Morrill, J., et al. (2002), Electron energy and electric field estimates in sprites derived from ionized and neutral N2 emissions, Geophys. Res. Lett., 29(10), 1462, doi:10.1029/2001GL014018.

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