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The location of the upward region 2 current sources (Iijima and Potemra 1976) inside the magnetosphere at comparatively small geocentric distances is well known.
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There is more than one upward current region in the evening sector: similarly, at earlier times, there had been more than one downward current region in the morning sector.
In this case, the upward sloping region encompasses four genes (VACV-COP E5R, E6R, E7R and E8R) and the two downward sloping regions flanking each side of this region encompass genes that are located on the bottom strand.
The fundamental difference between the two paradigms is the nature of the assumed upward ∇N region.
The current study discusses two aspects of ESWs: their characteristics in the magnetosheath, and their propagation in the magnetosheath and in the auroral acceleration (upward current) region.
From the auroral imaging, the upward current region was inferred to be west of ATH and would not have caused a Y component perturbation in the period prior to 09 10 UT.
The second type of propagation study uses striated Auroral Kilometric Radiation (SAKR) bursts, observed on multiple Cluster satellites, as tracers of ion solitary waves in the upward current region.
Their depths are deeper in the convex-upward seafloor region and shallower in the convex-downward seafloor region relative to the neighboring areas.
The digisonde observations (see Fig. 2) also do not provide evidence of large, long-lasting upward F-region uplifts for the three events discussed here.
While weaker upward F-region uplifts were observed on this day, the layer did not return to lower heights (h'F ∼ 250km) as it was observed on the other 2 days.
Innumerable layers of buoyancy-driven micro-convection in conjunction with conduction may operate to directionally bias and/or augment the flow of core-derived heat upward to regions of lesser density (Herndon 2011).
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