M. Conde et al., Assimilated observations of thermospheric winds, the aurora, and ionospheric currents over Alaska, J GEO R-S P, 106(A6), 2001, pp. 10493-10508
We present simultaneous measurements of thermospheric winds, auroral emissi
ons, and ionospheric currents over Alaska, obtained from four separate inst
ruments. Thermospheric (F region) wind maps were recorded by an all-sky ima
ging Fabry-Perot spectrometer located at Poker Flat and observing at lambda
630.0 nm. Auroral images at lambda 557.7 nm were obtained from the low-res
olution visible imager on board the Polar satellite. White-light all-sky au
roral images were recorded by ground-based all-sky cameras located in Alask
a at Poker Flat (65 degrees 07'N, 212 degrees 34'E) and at Kaktovik (70 deg
rees 06'N, 217 degrees 24'E). Finally, the east-west component of the ionos
pheric F region plasma convection was inferred using the Alaskan meridian c
hain of magnetometers. Montage images of these four data sets are presented
, projected onto a geographic map of the Alaskan region. We examine a 10-ho
ur period during the Alaskan local nighttime of February 10, 1997. These mo
ntages illustrate a close relationship between spatial structures occurring
in the aurora, in the ionospheric plasma convection, and in the F region w
ind field. Latitudinal shear of the geomagnetic zonal wind, often observed
in the premidnight time sector, was seen to be associated with both the equ
atorward and poleward boundaries of the discrete aurora. We focus particula
rly on a period commencing just after 0900 UT, when a strong shear in the z
onal wind was observed to sweep southward across Alaska. After magnetic mid
night the wind field was dominated by the emergence of the "cross-polar jet
" from the polar cap. This overwhelmed any wind features associated with lo
cal auroral processes.