HR: 0800h
AN: SM51B-0365 [Abstracts]
TI: The Cusp Aurora in the Conjugate Hemispheres of the Earth
AU: * Ostgaard, N
EM: Nikolai.Ostgaard@ift.uib.no
AF: Department of Physics and Technology,University of Bergen, Allegt 55, Bergen, N5007
Norway
AU: Mende, S B
EM: mende@ssl.berkeley.edu
AF: Space Sciences Laboratory, University of California, Berkeley, 7 Gauss Way, Berkeley, CA 94720
United States
AU: Frey, H U
EM: hfrey@ssl.berkeley.edu
AF: Space Sciences Laboratory, University of California, Berkeley, 7 Gauss Way, Berkeley, CA 94720
United States
AU: Immel, T J
EM: immel@ssl.berkeley.edu
AF: Space Sciences Laboratory, University of California, Berkeley, 7 Gauss Way, Berkeley, CA 94720
United States
AU: Sigwarth, J B
EM: john.b.sigwarth@nasa.gov
AF: NASA Goddard Space Flight Center
Electrodynamics Branch, Code 696, Building 21, Greenbelt, MD 20771
United States
AU: Frank, L A
EM: louis-frank@uiowa.edu
AF: Department of physics and astronomy, University of Iowa, Iowa City, Iowa, IA 52242-1479
United States
AB:
In this paper we examine the Earth's cusp aurora associated with high latitude
lobe reconnection. The cusp aurora is observed simultanously in both
the southern and northern hemispheres in similar wavelengths by the
cameras on IMAGE and Polar satellites. Due to the high solar wind pressure both
the proton and electron aurorae are fairly bright, dominated by ~8 keV
protons and 0.5-1 keV electrons. As predicted by theory, the
longitudinal asymmetric location of the cusp aurora is strongly
controlled by the IMF By component. The southern cusp aurora is
observed several degrees poleward of the northern cusp aurora and can
be attributed to either a tilt effect or an IMF Bx effect. These rare
observations also confirm our earlier findings that theta aurora can be
a non-conjugate phenomenon controlled by the IMF Bx component.
DE: 2704 Auroral phenomena (2407)
DE: 2724 Magnetopause, cusp, and boundary layers
DE: 2740 Magnetospheric configuration and dynamics
DE: 2784 Solar wind/magnetosphere interactions
SC: SPA-Magnetospheric Physics [SM]
MN: 2004 AGU Fall Meeting