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#27.     Auroral Images

  (Files in red–history)


25. Auroral Currents

25H. Birkeland Currents

25a. Triad

25b. Io Dynamo

25c. Space tether

26. Polar Caps

26H. Birkeland, 1895

27. Aurora from Space

28. Aurora Origin

28a. Plus and Minus

29. Low Polar Orbit

30. Magnetic Storms

30a. Chicago Aurora
        While the aurora is plainly visible to the eye, it changes constantly. A camera is therefore a useful tool in studying its features. For instance, how high up is the aurora? In principle, two observers on the ground can tell, by comparing the position of the same auroral arc against the background stars. In practice, only photographs snapped at exactly the same instant give satisfactory accuracy. The method was pioneered by Martin Brendel in 1892 and was greatly expanded by Carl Stoermer around 1910; it turned out that auroras occured most frequently around 100 km (60 miles), though much higher auroras (usually red) were also sometimes seen     During the International Geophysical Year 1957-8, "all-sky cameras" were devised to record the entire aurora, horizon to horizon, by photographing its reflection (rather distorted!) from a curved mirror. But the best view is still from space. Starting in 1968, military satellites of the DMSP series scanned the land below them, their sensor sweeping again and again from far left to far right, perpendicular to their orbit. As the minutes passed, the scanned strips added up to full images, which often included auroral arcs.

        The picture on the right is an example of such an image, showing the bright aurora of the great magnetic storm of 14 March, 1989. The display stretches across Canada; just below it, in the middle of the picture, are the lights of Chicago, next to Lake Michigan. Other US cities are also visible, Florida is outlined and so is Hudson Bay, near the top of the picture.

Scientific Imagers in Space

    The Canadian scientific satellite Isis-2 (1971) carried an auroral imaging camera and discovered the diffuse aurora, a broad ribbon around the auroral oval, too spread-out to be noticed from the ground. This aurora is probably formed by electrons which leak out of the ends of field lines threading the plasma sheet.

    More comprehensive observations of the aurora from above were carried out (1981 - 1987) by the Dynamics Explorer 1 (DE-1) satellite which moved in an elongated polar orbit rising to 4.65 RE. Several modes of operation were used; some pictures were taken in the greenish oxygen "line" (emitted at the precise wavelength of 5577 angstrom) which usually dominates the aurora's appearance from the ground, but many used the ultra-violet. The typical time resolution was 2-12 minutes, enough to resolve the phases of a substorm but not finer details.

    Later auroral imagers included Sweden's "Viking" (in 1986) and " Freja." Currently, NASA's Polar (1996) collects images of the polar aurora using three cameras--in visible light (sometimes as frequently as 12 seconds apart), in ultra-violet and in x-rays.

Theta Aurora

    DE also studied a special class of auroras (mapped earlier by Isis 2), aligned not with the auroral oval but sticking out from it, into the dark interior around the magnetic pole, generally aligned with the sunward direction. They occur at quieter times, away from substorms. The DE imaging camera found that at times such arcs extended completely across the oval, bridging the dark space from the night side to the day side. The global pattern then resembled the Greek letter theta, a circle with a bar across its middle (Θ), and this form was therefore named the "theta aurora." No good explanation exists as yet for either sunward arcs or the theta aurora.

The Speed of Auroral Motions

    While satellite imagers view the aurora from above, TV cameras are nowadays used to watch it from below, a narrower view than the one from space but a more detailed one. To the eye the aurora appears quite sluggish, its rays slowly brightening and fading. However, the slowness is not in the aurora but in the light emission process of the green line of oxygen, which usually provides most of the auroral light seen from the ground. An oxygen atom energized by the collision of an auroral electron may not emit this light promptly, but only after a delay, typically close to a second.

    Sensitive TV cameras can filter out that light and view the aurora in other emissions, fainter but responding much more promptly. The resulting pictures show more details and change quite rapidly.

Questions from Users:
            ***     Skywriting by Aurora?

Next Stop: #28.  Auroral Acceleration

Last updated 14 December 2004
Re-formated 13 March 2006