ESR Radar data for 2002/01/17

Spectra from ESR RTG

These are the standard spectra produced by the on-site raw data visualisation program, called rtg. These figures show the 5-second integrated data taken through the ordinary ESR receiver system.

Beware that in these plots, and all plots from the ESR rtg, the frequency axis is inverted, i.e. upshifted frequencies are to the left.
Header Header Header Header
06:45:55 UT: spectra 1 spectra 2
06:46:00 UT: xxx spectra 2
06:46:05 UT: xxx spectra 2
06:46:10 UT: xxx spectra 2
06:46:15 UT: xxx spectra 2
06:46:20 UT: xxx spectra 2
06:46:25 UT: xxx spectra 2
06:46:30 UT: xxx spectra 2
06:46:35 UT: xxx spectra 2


Some interferometry results

Plot for the 0.5 second integration starting at 06:46:20.50 UT. Full-size plot in Encapsulated PostScript or PDF also available.

From the raw timeseries, we compute powerspectra from each of the two antennas, and the cross-spectrum, which, when normalised, gives the coherence, and also the phase. This is explained in more detail on a separate page.

When plotting these quantities for all available ranges, we obtain a colourplot like the figure to the right. Left to right, top to bottom, the panels are:

Powerspectra has been computed in (mostly) the same way as is done in the ordinary ESR receiver system, cross-spectra in the same way, but extended to cover negative lags.

Time development

Development of power (in dB) vs. time for three different range regions. Blue lines for upshifted and red lines for downshifted power. (EPS or PDF)

To see how the event develops in time, we have made plots of power and coherence vs. time. For power, we have separated the covered range into three intervals, and extracted the maximum power per unit frequency and unit range from each interval, separately for up- and down-shifted frequencies.

The figure on the right shows the development of power. We can see how both shoulders increase by two orders of magnitude within one second, and how the downshifted shoulder stays higher as the upshifted shoulder weakens, and that the downshifted shoulder remains higher throughout most of the event.

Since we have not performed background subtraction or range2 correction, power from different ranges (or range intervals) should not be compared directly.

Development of coherence vs. time for different range regions. Blue lines for upshifted and red lines for downshifted frequencies. (EPS or PDF)

The figure on the right shows development of coherence vs. time. It is like the figure above.

There are a couple of caveats with this figure also: No attempt has been made at distinguishing spurious (false) coherences from those that are likely to show real coherent scattering structures. From a single coherence plot (like the third panel of the four-panel plots above) it is relatively simple to assess the noise level of the coherence. This is not so easy from this summary plot. Furthermore, coherence is only extracted with no phase rotation (see below). Some of the coherent structures have been seen to be more prominent when phase rotation is applied.


Combined PAI images and radar spectra

FoV: The fields of view of the camera and radar shown in comparison (FieldsOfView.pdf)

When comparing the results from the radar with the optical measurements we must be careful, as the fields of view of the two instruments are not exactly the same. The leftmost drawing in figure FoV shows a situation where an auroral arc is situated outside the radar beam itself, but from the cameras field of view we would see auroral luminosity in the circle defined by the radar beam at 105 km alt. This could lead to false conclusions. The rightmost drawing shows the situation where an arc is situated within the radarbeam. If the cause of the enhanced radar echoes is associated with auroral luminosity (precipitating particles), then we should expect correlations between light intensity within the radarbeam (measured with the camera), and enhanced echoes.

Beams: The radar beam mapped to two different altitudes (PDF)

Due to the separation of the radar and the camera, the radar beam, when drawn in the cameras view, will move depending on the altitude we map it to, this is shown in figure Beams

We can compare the time development in the radar measurements, with the time development of the averaged intensity/pixel measured through the circle defined by the radarbeam at a certain altitude, to study the correlation between the two instruments. There is a very poor correlaTion in the two timeseries, and a probable cause of that is the separation of the two instruments. By studying the PAI movie sequences, we see that the situation outlined in the rightmost drawing in figure FoV (where the auroral arc ends up within the radarbeam), is occuring between 06:46:20 -- 06:46:22. This can also be identified from the lower panel of figure Comparison, where the broken line (averaged intensity/pixel in a ring surrounding the radarbeam) is much lower than the solid line (averaged intensity /pixel within the radarbeam). This short time period is interesting because we expects some correlation between the radar and optical measurements here. Obviosly, the correlation is still bad. However, it seems like the optical measurements is dragging behind the observed radar echoes (with less than a second). Asgeir reminded me about the green lines having about a 0.7 - 0.8 s. delay time. During this campaign, the PAI was not using any filter, and it is this state very sensitive to the green. Next thing to do is to test the correlation when a delay time of 0.7 - 0.8 s. is subtracted from the optical time serie.

Comparison: The upper panel shows the time development of the radar power vs. time for different range/frequency regimes, and the middle panel panel shows the max coherence, similar to earlier plots. The lower panel shows the development of the averaged intensity/pixel (arbitary units) measured by the camera in the circle defined by the radar beam at 105 km altitude (solid line). The broken lines shows the averaged intensity/pixel measured in a ring surrounding the radarbeam, with a radius twice as large as the radarbeam. (EPS or PDF)

SliceStack: (EPS or PDF)

Correlation2: (EPS or PDF)

Correlation1: (EPS or PDF)

BaseLine: (PDF)