Observation of IMF and seasonal effects in the location of auroral substorm onset

Details Observation of IMF and seasonal effects in the location of auroral substorm onset Observation of IMF and seasonal effects in the location of auroral substorm onset

Apr 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001jgr...106.5799l&link_type=abstract

Journal of Geophysical Research, Volume 106, Issue A4, p. 5799-5810

Physics

50

Magnetospheric Physics: Auroral Phenomena, Magnetospheric Physics: Solar Wind/Magnetosphere Interactions, Magnetospheric Physics: Storms And Substorms

Scientific paper

We use Polar ultraviolet imager (UVI) and Wind observations to study the location of 648 well-defined Northern Hemisphere auroral breakups (substorm onsets) in response to interplanetary magnetic field (IMF) orientation and season. The most likely onset location is at 2230 MLT and 67° Λm with half-maximum widths of 3 hours of MLT and 2° Λm, respectively. The onset latitude depends primarily on IMF Bz, but also Bx: the onset latitude decreases for Bx>0 or Bz<0 and increases for Bx<0 or Bz>0. The onset longitude depends on season and IMF By. In summer, substorms tend to occur in the early evening at ~2200 MLT, whereas in winter they tend to occur near midnight at ~2300 MLT. The average summer-winter difference in the onset location is ~1 hour of MLT. Large By effects on the onset longitude occur only when Bx and By are small. Onset locations shift toward earlier local times for By>0 and toward midnight for By<0. The average onset local time is earliest (2200 MLT) for By>0 in summer and latest (2330 MLT) for By<0 in winter. These dependencies coincide with those previously reported for the evening sector ionospheric zonal flow reversal in response to IMF By and season, indicating that auroral breakups are most likely in regions of large velocity shears. A weak dependence of the MLT onset location on the IMF Bx is identified: for Bx>0 the onset location shifts toward dusk when By>0 but toward dawn when By<0 the sense of this shift reverses for Bx<0. An implication of the results is that auroral breakup is not conjugate.

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