3rd LOIS Workshop, November 24-25, 2002
Växjö University, Växjö, Sweden
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Using LOFAR-LOIS for high-resolution radio
and radar studies of the effects of powerful
HF pumping into the nightside auroral ionosphere
on the substorm development
Nataly F. Blagoveshchenskaya
nata@aari.nw.ru
Arctic and Antarctic Research Institute
St. Peterburg, Russia
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Abstract
Recent experiments with the EISCAT HF Heating facility, located near
Tromsø, Norway, have indicated that HF pumping into the nightside auroral
ionosphere along the magnetic field-aligned direction produces a
modification of the magnetosphere-ionosphere coupling which, in turn,
under certain geophysical conditions may cause triggering of auroral
activation. Distinctive features related to auroral activation in
course of the Tromsø HF pumping experiments were identified in
multi-instrument ground-based observations.
These features include:
- Strong increase of the local ionospheric electric field
- Modification of the auroral arc and local spiral-like formation
- Extremely strong electron temperature enhancements in a wide altitute range
- Generation of intense ion outflows
A possible scheme for the substorm triggering
due to the excitation of the turbulent Alfvén boundary layer in the
ionospheric Alfvén resonator is considered. Still, many questions are
outstanding:
- How far out in the magnetosphere do the observed phenomena go?
- What do they produce in the magnetosphere?
- What is the role of plasma instabilities in the process?
Using a LOFAR-LOIS
combination for high-resolution deep-space radar observations would be
an extremely powerful tool to find answers to these questions.
The presentation (PDF)
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