Real and spurious anti-correlations between short-period variations of field-parallel and field-perpendicular plasma velocities in EISCAT data

Physics

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Eiscat Radar System (Europe), F Region, Magnetic Field Configurations, Plasma Dynamics, Geomagnetism, Oxygen Ions, Random Noise

Scientific paper

Measurement of the observed anticorrelation between the field-perpendicular component of F-region plasma velocity in the north-south plane and the downward, field-parallel component has been proposed as a way to determine the value of the O-O(+) collision frequency. However, ramdon noise errors in measurements of plasma velocity made at EISCAT may combine in analysis to induce a spurious anticorrelation between the derived values of these components, which is hard to distinguish from any genuine anticorrelation.

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