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Response of the ionospheric convection pattern to a rotation of the interplanetary magnetic field on January 14, 1988

Journal Article · · Journal of Geophysical Research; (United States)
DOI:https://doi.org/10.1029/92JA01731· OSTI ID:6902384
; ;  [1]
  1. Univ. of Texas, Richardson (United States)
Ionospheric convection signatures observed over the polar regions are provided by the DMSP F8 satellite. The authors consider five passes over the southern summer hemisphere during a time when the z component of the interplantary magnetic field was stable and positive and the y component changed slowly from positive to negative. Large-scale regions of sunward flow are observed at very high latitudes consistent with a strong z component. When B[sub y] and B[sub z] are positive, but B[sub y] is greater than B[sub z], strong evidence exists for dayside merging in a manner similar to that expected when B[sub z] is negative. This signature is diminished as B[sub y] decreases and becomes smaller than B[sub z] resulting in a four-cell convection pattern displaced toward the sunward side of the dawn-dusk meridian. In this case the sign of B[sub y] affects the relative sizes of the two highest-latitude cells. In the southern hemisphere the duskside high-latitude cell is dominant for B[sub y] positive and the dawnside high-latitude cell is dominant for B[sub y] negative. The relative importance of possible electric field sources in the low-latitude boundary layer, the dayside cusp, and the lobe all need to be considered to adequately explain the observed evolution of the convection pattern.
OSTI ID:
6902384
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 97:A12; ISSN JGREA2; ISSN 0148-0227
Country of Publication:
United States
Language:
English