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Letter

Nature 460, 491-493 (23 July 2009) | doi:10.1038/nature08154; Received 17 March 2009; Accepted 21 May 2009

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Asymmetric auroral intensities in the Earth's Northern and Southern hemispheres

K. M. Laundal1 & N. Østgaard1

  1. Department of Physics and Technology, Allegt 55, University of Bergen, N-5007 Bergen, Norway

Correspondence to: N. Østgaard1 Correspondence and requests for materials should be addressed to N.Ø. (Email: nikolai.ostgaard@uib.no).

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It is commonly assumed that the aurora borealis (Northern Hemisphere) and aurora australis (Southern Hemisphere) are mirror images of each other because the charged particles causing the aurora follow the magnetic field lines connecting the two hemispheres. The particles are believed to be evenly distributed between the two hemispheres, from the source region in the equatorial plane of the magnetosphere. Although it has been shown that similar auroral features in the opposite hemispheres can be displaced tens of degree in longitude1, 2 and that seasonal effects can cause differences in global intensity3, 4, the overall auroral patterns were still similar. Here we report observations that clearly contradict the common assumption about symmetric aurora: intense spots are seen at dawn in the Northern summer Hemisphere, and at dusk in the Southern winter Hemisphere. The asymmetry is interpreted in terms of inter-hemispheric currents related to seasons, which have been predicted5, 6 but hitherto had not been seen.

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