4.3 Article

Large-scale observations of a subauroral polarization stream by midlatitude SuperDARN radars: Instantaneous longitudinal velocity variations

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AMER GEOPHYSICAL UNION
DOI: 10.1029/2011JA017232

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  1. GEM from the National Science Foundation [ATM-0924919]
  2. Deutsches Zentrum fur Luft- und Raumfahrt [50OC1102, 50OC1001]
  3. National Science Foundation [ATM-0838219, ATM-0946900, ATM-0838356, ATM-0838142, ATM-0838270]
  4. Directorate For Geosciences
  5. Div Atmospheric & Geospace Sciences [0946900, 946902] Funding Source: National Science Foundation
  6. Div Atmospheric & Geospace Sciences
  7. Directorate For Geosciences [0856093, 0838219] Funding Source: National Science Foundation

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We present simultaneous measurements of flow velocities inside a subauroral polarization stream (SAPS) made by six midlatitude high-frequency SuperDARN radars. The instantaneous observations cover three hours of universal time and six hours of magnetic local time (MLT). From velocity variations across the field-of-view of the radars we infer the local 2D flow direction at three different longitudes. We find that the local flow direction inside the SAPS channel is remarkably constant over the course of the event. The flow speed, however, shows significant temporal and spatial variations. After correcting for the radar look direction we are able to accurately determine the dependence of the SAPS velocity on magnetic local time. We find that the SAPS velocity variation with magnetic local time is best described by an exponential function. The average velocity at 00 MLT was 1.2 km/s and it decreased with a spatial e-folding scale of two hours of MLT toward the dawn sector. We speculate that the longitudinal distribution of pressure gradients in the ring current is responsible for this dependence and find these observations in good agreement with results from ring current models. Using TEC measurements we find that the high westward velocities of the SAPS are - as expected - located in a region of low TEC values, indicating low ionospheric conductivities.

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