Discussions of Observations
The geographical distribution of EDAC events is clear from the world map in the above figure.
The observations by the CPD instrument clearly reveals the dominant regions of energetic
radiation, the South-Atlantic anomaly (SAA) region, and the northern and southern auroral
zones. After analysis of the CPD data we can more precisely distinguish the cases on basis
of the radiation characteristics.
In the South-Atlantic anomaly region the magnetic field is weaker than in other regions of
the world with the result that the radiation belts come closer to the Earth and may reach
down to the altitude of the satellite (640-880 km). For the SAA cases the CPD instrument
measures high fluxes of hard, penetrating radiation which is most likely protons and
electrons in the MeV range.
For the auroral zone cases the CPD instrument measures low to moderate fluxes of high-energy
radiation, much less than in the SAA cases. The charged particles causing the events are
probably softer than the CPD range starting at 50 keV. Hence the events are more likely
related to dielectric charging by intense fluxes of low energy particles than to penetrating
high-energy particles.
There was this grouping based on data for 82 events from April-August,1999 :
SAA cases: 46 EDAC events
Auroral Zones: 21 EDAC events
Other regions: 15 EDAC events
For the SAA cases there is a clear altitude variation of the cases. The satellite altitude
varies between 640 and 880 km. Dividing this range into three subranges we obtain:
640-720 km: 11 EDAC cases
720-800 km: 10 EDAC cases
800-880 km: 25 EDAC cases
Hence, the risk of being exposed to hard radiation in the South-Atlantic Anomaly region
increases dramatically with height just above 800 km.
For the SIM cases there is a corresponding clustering of events within the SAA region.
This has some serious consequences for the worldwide mapping of the geomagnetic
field by the Oersted satellite. Generally there is much less magnetic vector data
available in this highly interesting region than in other regions of the world. However,
the altitude dependence of SIM unavailability corresponds to that for the EDAC event
outlined above. Accordingly one should look for orbits where the perigee is over the
SAA region. The orbit cycle of around 3 months is clearly seen in long-term recordings
of SIM availability
Modeling of EDAC bit flip events
We have attempted to model the occurrences of bit flips detected by the EDAC system by
using the radiation model of the ESA/NASA Space Environment Information System (SPENVIS)
(Heynderickx, D., B. Quaghebeur, E. Speelman, Space Environment Information Service
( http://www.spenvis.oma.be/spenvis/ ).
For the S-RAM memory component Micron MT5C1008C-35-L883C we have a Single Event Upset
(SEU) Linear Energy Transfer (LET) threshold of ~3 MeV cm2/mg and a radiation cross
section of 2 10-2 cm2 . The CDH1 and CDH2 S-RAM memory circuits are mounted in
electronics boxes at the middle of the satellite body. We have derived approximate
shieldings for the two CDH units (3.50 and 2.0 g/cm2). Using the SPENVIS web service
we have then derived the LET spectra for typical Ørsted satellite orbits. These
spectra provide integral fluxes above the LET threshold of particles capable of
producing SEU in the circuit. Multiplying these fluxes with the device cross section
and the exposure solid angles gives the anticipated SEU rates. They are shown in the
table below.
Table. Comparison of predicted (SPENVIS) and observed (Ørsted) Single Event Upsets