Articles | Volume 33, issue 3
Ann. Geophys., 33, 333–344, 2015
Ann. Geophys., 33, 333–344, 2015

Regular paper 17 Mar 2015

Regular paper | 17 Mar 2015

Outflow of low-energy O+ ion beams observed during periods without substorms

G. K. Parks1, E. Lee2, S. Y. Fu3, M. Fillingim1, I. Dandouras4, Y. B. Cui3, J. Hong2, and H. Rème4 G. K. Parks et al.
  • 1Space Sciences Laboratory, University of California, Berkeley, CA, USA
  • 2School of Space Research, Kyung Hee University, Yongin, Gyeonggi, Korea
  • 3School of Earth and Space Sciences, Peking University, Beijing, China
  • 4CNRS, IRAP, 9 Ave. Colonel Roche, Toulouse, France

Abstract. Numerous observations have shown that ions flow out of the ionosphere during substorms with more fluxes leaving as the substorm intensity increases (Wilson et al., 2004). In this article we show observations of low-energy (few tens of electron volts) ionospheric ions flowing out periods without substorms, determined using the Wideband Imaging Camera (WIC) and Auroral Electrojet (AE) indices. We use Cluster ion composition data and show the outflowing ions are field-aligned H+, He+ and O+ beams accelerated to energies of ~40–80 eV, after correcting for spacecraft potential. The estimated fluxes of the low-energy O+ ions measured at ~20 000 km altitude are >103–105 cm−2 s. Assuming the auroral oval is the source of the escaping ions, the measured fluxes correspond to a flow rate of ~1019–1021 ions s−1 leaving the ionosphere. However, periods without substorms can persist for hours suggesting the low-energy ions flowing out during these times could be a major source of the heavy ion population in the plasma sheet and lobe.

Short summary
Ions from Earth's ionosphere continually escape into space. This article examines ions escaping the auroral oval, a region in the polar region of Earth where auroras occur. Previous works have shown that ionospheric ions escape during active auroras, and more as the intensity of the aurora increases. In contrast, we have examined times of no auroras and find that ions are still escaping the auroral ionosphere. These escaping ions are an important source of auroral ions in the magnetosphere.