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Frequency dependent power ¯uctuations: a feature of the ESR system or physical?
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Frequency dependent power fluctuations: a feature of the ESR system or physical?
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Types of pulsating aurora: comparison of model and EISCAT electron density obser...
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Naturally enhanced ion-acoustic lines at high altitudes
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Naturally enhanced ion-acoustic lines at high altitudes
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Observations of diverging field-aligned ion flow with the ESR
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Ion upflow and downflow at the topside ionosphere observed by the EISCAT VHF rad...
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Ion upflow and downflow at the topside ionosphere observed by the EISCAT VHF rad...
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Aspect angle sensitivity of pump-induced optical emissions at EISCAT
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Ion up¯ow and down¯ow at the topside ionosphere observed by the EISCAT VHF radar...
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Particle precipitations during NEIAL events: simultaneous ground based observati...
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based observations at Svalbard
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Plasma line observations from the EISCAT Svalbard Radar during the International...
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Extreme ion heating in the dayside ionosphere in response to the arrival of a co...
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Lower-thermospheric wind fluctuations measured with an FPI during pulsating auro...
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Study on spatiotemporal variations of ionospheric trough in auroral/subauroral r...
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Survey of conditions for artificial aurora experiments by the second electron gy...
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Survey of conditions for artificial aurora experiments at EISCAT Tromsø using dy...
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Substorm topology in the ionosphere and magnetosphere during a flux rope event i...
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www.ann-geophys.net/25/661/2007/ © European Geosciences Union 2007
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Related Subjects
Q
Science
Geophysics. Cosmic physics
Physics
QC1-999
QC801-809
Geology
Artificial aurora
Dynasonde
EISCAT
G
Geodesy
Geography. Anthropology. Recreation
Ionospheric heating
Plasma waves and instabilities
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QE1-996.5
Tromsø
Aspect angle
ENHANCED AIRGLOW
Environmental pollution
Environmental protection
Environmental sciences
FREQUENCY
GE1-350
Geosciences
HEATER
HF
IRREGULARITIES
Ionosphere
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