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When a bright aurora is seen in the auroral zone, a strong magnetic disturbance is usually also observed there. The disturbing magnetic field can be much stronger than that of a magnetic storm but it is strictly local, fading away quickly as one moves equatorward. This limited extent suggests that the currents which disturb the field flow somewhere nearby, probably near the auroral arcs. The Norwegian Kristian Birkeland, who carefully observed auroral disturbances around the turn of the century, concluded that those currents flowed parallel to the ground, along the auroral formation.
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| Any electric current, however, must flow in a closed
circuit, and since it seemed to be caused (like that of the aurora) by processes taking place in distant space, Birkeland proposed that it came down from space at one end of the arc and returned to space at the other end. The drawing below illustrates the idea and was taken from Birkeland's 1903 report on his
expeditions to the auroral zone:
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 Waterloo Bridge experiment
| Faraday understood this very well. Knowing that water conducted electricity (because of dissolved salts), he tried in 1831 to observe such a dynamo experimentally. He strung a wire along Waterloo bridge in London and dipped its ends into the river at two separated points, so that its circuit could be completed through the flowing water. He then tried to measure the electric current generated by the river's flow through the magnetic field.
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The idea was sound, but the current was too weak to be measured by him.
Faraday nevertheless speculated that the aurora (which he believed to be an
electric phenomenon) might be powered in a similar way by the Gulf Stream
flowing to the north-east through the Atlantic Ocean, beginning just offshore
from the US. Of course, what Faraday forgot here was that to connect the ocean to the aurora, the current would have to cross the lower atmosphere, which is an excellent insulator and would block its flow. An interesting dynamo of this type exists between the planet Jupiter and its innermost big moon Io (click for details). The space shuttle can also generate electric power that way (at the expense of its orbital energy), using a long wire dangling from it into space. Such a space tether experiment was conducted aboard the space shuttle Columbia on 25 February, 1996, ending unexpectedly when the tether suddenly broke. Sir Joseph Larmor in England first proposed in 1919 that dynamos consisting entirely of fluids might explain the creation of sunspot magnetic fields. His idea was that as solar plasma flowed through magnetic fields, dynamo effects produced the very same currents which also created those magnetic fields. Because this is a process which "lifts itself by its own bootstraps" (the magnetic fields needed by the dynamo are produced by the electric currents which are its output), it must build up gradually, starting from some "seed" magnetic field of a different source. Such a "dynamo mechanism" was also believed to be the source of the magnetic field arising inside the Earth's molten core. It is impossible to observe that region directly, but in 1964 Stanislaw Braginskii, in Russia, mathematically demonstrated a possible class of such "dynamos." The slow decade-by-decade variation of the Earth's field probably comes from slow changes in the flow patterns of the core - not, as Halley once proposed, from magnetized spherical layers, one inside the other, all rotating differently.
If the bundle of open lines maps to the region inside the auroral oval, it can be shown that the "dynamo currents" from the above process flow earthward on the morning side of the magnetic pole and spaceward on the evening side. One might guess that the circuit would be completed by connecting the two flows across the polar ionosphere, from the morning side, to the evening side (drawing below).
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| When in 1973 the navy satellite Triad (see history) flew through this region
in a low-altitude orbit, its magnetometer indeed detected the signatures of two
large sheets of electric current, one coming down on the morning side of the
auroral zone, one going up on the evening side, as expected. Because Kristian
Birkeland had proposed long before currents which linked Earth and space in this fashion, they were named Birkeland currents (by Schield, Dessler and Freeman, in a 1969 article predicting some of the features observed by Triad). Typically, each sheet carries a million amperes or more.
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But that wasn't all. Equatorward of each current sheet, Triad noted a
parallel sheet almost as intense, flowing in the opposite direction: those field lines were no longer open, but closed inside the magnetosphere. It thus seemed that most of the electric current coming down from space (about 80%) did not choose to close through the ionosphere across the magnetic poles. Rather, it found an alternate way: it flowed in the ionosphere a few hundred miles equatorward and then headed out again to space, where the currents (presumably) found an easier path.
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A 1976 study by Takesi Iijima and Tom Potemra used Triad data to map the
average "footprints" of these sheets in the polar ionosphere, including their
intricate overlap at midnight. Their result is plotted below: the map is centered at the northern magnetic pole (though southern data were combined to produce this graph), midnight is at the bottom, and noon (where some minor additional currents exist) is at the top. Dark shading indicates currents flowing towards Earth, light shading, currents flowing outward into space.
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