| Total number of nights with useful Io images: |
|
| Number of nights where images have been visually inspected and for which large outbursts could have been detected: |
|
| Number of large outbursts seen in images and photometry: |
|
| Number of nights when other, fainter, hotspots were seen (excluding Loki): |
|
The primary purpose of this program is to detect the brightest Io eruptions, termed "outbursts". These events are the most likely to have an effect on Io's surface or Jupiter's magnetosphere, but are too brief to have much chance of being detected by Galileo itself. They are also too brief for the IRTF Galileo support program to detect most of them, but any that it does detect during the Galileo mission can be correlate with Galileo remote sensing and magnetospheric data.
By the luck of the draw, we have detected one outburst on 95/09/27,
shortly after this program started (thus demonstrating the program's
outburst-detecting capabilities), but only one has been seen during
the Galileo orbital tour which started in December 1995, that one was first
detected by Bob Howell at WIRO and observed at the IRTF following his notifying
the TOs. We have added considerably to the knowledge of outburst
frequency
(important for assessing Io resurfacing rates: Blaney et al. 1995,
"Volcanic eruptions on Io: Heat flow, resurfacing, and lava
composition", Icarus 113, 220), as shown in the following
table:
| Observers |
|
|
Outbursts Seen |
| Witteborn et al. |
|
|
|
| Sinton et al. |
|
|
|
| Johnson et al. |
|
|
|
| Spencer et al. |
|
|
|
| Howell et al. |
|
|
|
| IRTF Galileo support |
|
|
|
| Totals |
|
|
This table does not include the August 1999 outburst, as it was only observed by NSFCAM because an outburst was known to be occurring. The Galileo support program has provided 25% of the data in this table, and has detected 28% of all outbursts ever seen (including the August 1999 event): substantial contributions for a ten-minute-per-night program.
The other, fainter, hot spots that have been detected by this program require more image analysis than has been done so far for accurate determination of locations and fluxes, but the data are available for this work to be done when time permits.