Cluster observations of the high-latitude magnetopause and cusp: initial results from the CIS ion instruments

Academic Article

Abstract

  • Abstract. Launched on an elliptical high inclination orbit (apogee: 19.6 RE) since January 2001 the Cluster satellites have been conducting the first detailed three-dimensional studies of the high-latitude dayside magnetosphere, including the exterior cusp, neighbouring boundary layers and magnetopause regions. Cluster satellites carry the CIS ion spectrometers that provide high-precision, 3D distributions of low-energy (<35 keV/e) ions every 4 s. This paper presents the first two observations of the cusp and/or magnetopause behaviour made under different interplanetary magnetic field (IMF) conditions. Flow directions, 3D distribution functions, density profiles and ion composition profiles are analyzed to demonstrate the high variability of high-latitude regions. In the first crossing analyzed (26 January 2001, dusk side, IMF-BZ < 0), multiple, isolated boundary layer, magnetopause and magnetosheath encounters clearly occurred on a quasi-steady basis for ~ 2 hours. CIS ion instruments show systematic accelerated flows in the current layer and adjacent boundary layers on the Earthward side of the magnetopause. Multi-point analysis of the magnetopause, combining magnetic and plasma data from the four Cluster spacecraft, demonstrates that oscillatory outward-inward motions occur with a normal speed of the order of ± 40 km/s; the thickness of the high-latitude current layer is evaluated to be of the order of 900–1000 km. Alfvénic accelerated flows and D-shaped distributions are convincing signatures of a magnetic reconnection occurring equatorward of the Cluster satellites. Moreover, the internal magnetic and plasma structure of a flux transfer event (FTE) is analyzed in detail; its size along the magnetopause surface is ~ 12 000 km and it convects with a velocity of ~ 200 km/s. The second event analyzed (2 February 2001) corresponds to the first Cluster pass within the cusp when the IMF-BZ component was northward directed. The analysis of relevant CIS plasma data shows temporal cusp structures displaying a reverse energy-latitude "saw tooth" dispersion, typical for a bursty reconnection between the IMF and the lobe field lines. The observation of D-shaped distributions indicates that the Cluster satellites were located just a few RE from the reconnection site.Key words. Magnetospheric physics (magnetopause, cusp, and boundary layers; magnetosheath) Space plasma physics (magnetic reconnection)
  • Authors

  • Bosqued, JM
  • Phan, TD
  • Dandouras, I
  • Escoubet, CP
  • Reme, H
  • Balogh, A
  • Dunlop, MW
  • Alcayde, D
  • Amata, E
  • Bavassano-Cattaneo, MB
  • Bruno, R
  • Carlson, C
  • DiLellis, AM
  • Eliasson, L
  • Formisano, V
  • Kistler, Lynn
  • Klecker, B
  • Korth, A
  • Kucharek, Harald
  • Lundin, R
  • McCarthy, M
  • McFadden, JP
  • Mobius, E
  • Parks, GK
  • Sauvaud, JA
  • Status

    Publication Date

  • 2001
  • Keywords

  • magnetic reconnection
  • magnetopause, cusp, and boundary layers
  • magnetosheath
  • magnetospheric physics
  • space plasma physics
  • Digital Object Identifier (doi)

    Start Page

  • 1545
  • End Page

  • 1566
  • Volume

  • 19
  • Issue

  • 10-12