Rf. Pfaff et al., WAVE-VECTOR OBSERVATIONS OF THE 2-STREAM INSTABILITY IN THE DAYTIME EQUATORIAL ELECTROJET, Geophysical research letters, 24(13), 1997, pp. 1671-1674
Detailed measurements of electric field wavevectors of the Farley-Bune
man two-stream instability in the daytime equatorial electrojet were g
athered on a sounding rocket flown from Alcantara, Brazil. Primary two
-stream waves were detected in the altitude region of 104 - 108 km, wh
ere the current density and polarization electric field maximized and
where intense 3 m vertical echoes were observed by a 50 MHz backscatte
r radar. The in-situ measured wave components are predominantly orient
ed in the horizontal, zonal direction. Spaced receivers reveal wavelen
gths of 11-14 m with phase velocities of about 370 m/s at the peak wav
e power near 106.5 km. These velocities are constant from 1-15 m, indi
cative of dispersionless flow. Although the neutral wind was not measu
red, the in-situ phase velocity appears to be below that predicted by
linear theory.