HR: 0800h
AN: SA21C-0372 [Abstracts]
TI: Polar cap Artificial Auroras
AU: * Kosch, M
EM: m.kosch@lancaster.ac.uk
AF: Communication Systems, Lancaster University, Lancaster, LA1 4WA
United Kingdom
AU: Pedersen, T
EM: todd.pedersen@hanscom.af.mil
AF: Air Force Research Laboratory, Hanscom Air Force Base, Boston, MA 01731
United States
AU: Robinson, T
EM: txr@ion.le.ac.uk
AF: Dept. Physics & Astronomy, University of Leicester, Leicester, LE1 7RH
United Kingdom
AB:
It is well established that high-power high-frequency radio waves, when beamed into the F-layer ionosphere, accelerate
electrons 1-2 orders of magnitude above thermal levels. These electrons collide with the neutral oxygen atoms and nitrogen
molecules, which subsequently produce optical emissions identical to those in natural auroras. Artificial optical emissions
are one of few methods available to directly detect energetic electrons in the ionosphere. The mechanism of acceleration
remains under debate but there is evidence for turbulent upper-hybrid and Langmuir electrostatic waves. Artificial optical
emissions have been observed at low latitudes (e.g. Arecibo in Puerto Rico), mid-latitudes (e.g. SURA in Russia), and at high
latitudes (e.g. EISCAT in Norway and HAARP in Alaska). The electron accelerating mechanisms are sensitive to the magnetic
field aspect angle to the pump beam, hence the need to reproduce the phenomenon at different latitudes. Here we report on the
first attempt within the polar cap using the SPEAR facility on Svalbard, where the magnetic dip angle is only 8 degrees.
Svalbard also has the unique situation of being under the cusp during the daytime whilst the ground is in total darkness
during the winter months. In addition, Svalbard is the only location currently available where in-situ rocket measurements
are possible within an artificial aurora. Plans for a future launch are discussed.
DE: 2403 Active experiments
DE: 2407 Auroral ionosphere (2704)
DE: 2451 Particle acceleration
DE: 2483 Wave/particle interactions
SC: SPA-Aeronomy [SA]
MN: 2004 AGU Fall Meeting