Ionosphere
- Space-based
- DMSP cross polar cap voltages ~ 120 kV (M. Hairston)
- DMSP and NOAA particles indicate expanded auroral oval
(Data: F. Rich and D. Evans, Interpretations: D. Knipp)
- Ground-based
- SuperDARN coherent scatter radars observe large convection flow speed
enhancements and overall expansion of convection pattern in afternoon
sector (M. Rouhoniemi and K. Baker)
- Millstone Hill Incoherent Scatter Radar recorded prompt onset of
precipitation-produced ionization at lower F-Region heights
near L = 4 in evening sector and development of deep ionization
trough at L = 3.5. Hard precipitation was indicated in the region
of L = 4 which coincided with depletion of outer zone radiation belt
particle precipitation (dumping) observed by SAMPEX
(J. Foster)
- Evening substorm absorption event observed by Sondrestrom riometer
began near 23 UT (P. Stauning)
- 1000 nT bays observed by ground magnetometers in Mag 210 deg Chain
(Yumoto and K. Shiokawa)
- 500- 800 nT bays observed by IMAGE and Greenland Magnetometer Arrays
(H. Leuhr, E. Friis-Christensen P. Stauning and T. Morreto)
- 300-500 nT bays observed by CANOPUS and MACCS Magnetotmer Arrays in
North America (G. Rostoker and J. Hughes)
- Induced currents of 10-15 Amps flowed in 400 kV transformer at
Perttikowski Finland (A Viljanen)
- Voltages fluctuations in trans-oceanic cables began
(L. Lanzarotti)
- Ionospheric Mapping
- Auroral Oval underwent dramatic
expansion
- Cross polar cap voltage peak near 100 kV
(D. Knipp, B. Emery and J. Freeman)
- Polar Cap Voltage drooped momentarily to 112 kV at 2354 UT and
then began another rise (D. Weimer)
--Revised, Wednesday, 24 July 1996 by
bill@ncar.ucar.edu