HR: 09:10h
AN: SM21A-05 INVITED [PDF]
TI: The Structure and Dynamics of Poynting Flux in the Geomagnetic Tail and its Role in Generating
Aurora
AU: * Wygant, J R
EM: wygant@ham.space.umn.edu
AF: University of Minnesota, 116 Church St. SE, Minneapolis, MN 55455
AB:
Recent observations from the Polar and Cluster spacecraft have provided evidence that a variety of processes observed in
different locations in the geomagnetic tail during intervals of strong magnetic activity generate intense Alfvenic and
steady state Poynting flux directed along magnetic field lines towards the Earth. This Poynting flux is often capable of
providing the power necessary for the acceleration of auroral electrons and creating intense auroral displays. Strong
electric and magnetic fields associated with MHD waves carrying Poynting flux directed towards the Earth are observed in
the high beta plasma sheet near 9 Re during repetitive intervals of magnetic field dipolarization during major geomagnetic
storms. Intense Poynting flux associated with Alfvenic surface waves have been also been observed in the low beta Plasma
sheet boundary layer (PSBL) at altitudes of 4-7 Re immediately above the auroral acceleration region near the poleward
boundary of the auroral zone. During the main phase and peak of major geomagnetic storms, measurements of electric and
magnetic fields from Polar in the near Earth equatorial plasma sheet show evidence for spatially extensive (1-3 Re) regions
of intense Poynting flux (both steady state and Alfvenic) towards the Earth. This Poynting flux maps to low latitudes over
widths of 2-5 degrees. Finally, observations from the Cluster spacecraft studies demonstrate that strong Poynting flux is
radiated from the reconnection region near ~20 Re in association with magnetic field energy conversion in the tail. The
in-situ values of Poynting flux from these regions are 0.1 to 1.0 mW/m2 and may be related to the observations in the PSBL
The value of Poynting flux mapped to altitudes of 100 km are on the order 10-100 mW/m2 and are sufficient to power some
of the most intense aurora observed in the Polar spacecraft UV Image and the IMAGE spacecraft WIC data sets. The properties
of the structure and dynamics of the MHD waves associated with the Poynting flux will be summarized and compared to the
temporal and spatial structure of the auroral forms simultaneously observed by the IMAGE and Polar Space based imagers.
DE: 2704 Auroral phenomena (2407)
DE: 2740 Magnetospheric configuration and dynamics
DE: 2744 Magnetotail
DE: 2764 Plasma sheet
SC: SPA - Magnetospheric Physics [SM]
MN: 2003 Fall Meeting