Its was like watching someone turn off the life-support machines of an old friend. June 30th, 2008, was the last day of mission operations for the Ulysses spacecraft, after nearly 18 years of service. It also brings to an end the exploration of a region of our solar system that’s not likely to be visited again in our lifetimes.

The Ulysses Mission was originally conceived as the International Solar Polar Mission, a tandem mission with one spacecraft being built by NASA and the other by ESA. Budget cuts reduced the mission to a single spacecraft jointly engineered by the two agencies. Ulysses was originally to be launched in 1983, but was delayed to the Spring of 1986 and set to deploy from the cargo bay of the Space Shuttle Challenger. As a result of the Challenger accident, its launch was delayed even more. These delays would come back to haunt the mission as the radioisotope thermoelectric generators (RTGs) used to power the mission have a fixed lifetime and were constructed and tested in the early 80s. Ulysses was finally launched and deployed from the cargo bay of the Space Shuttle Discovery on October 6th, 1990 and began is trek out to Jupiter and to the Sun’s polar regions.

The primary 6-year mission called for a single solar orbit giving coverage of both the Sun’s southern and northern polar regions at solar minimum and covering radial distances from its perihelion of 1.3 AU to its aphelion of 5.4 AU. Ulysses performed so well that its mission would be extended multiple times allowing it to complete three full orbits. The additional orbits allowed Ulysses to investigate the polar regions during solar maximum, and during our current rise to maximum.

Eventually, the old RTGs became a terminal factor for the spacecraft. With power from the RTGs dwindling, power sharing techniques had to be employed. Various power sharing schemes were developed, but the one that was used allowed all of the science missions to remain active, however it required that the high-bandwidth X-band transmitter be shut down during data collection. Data was to be stored on board for later download. To retrieve data, the science instruments would be shut down and the transmitter restarted. However, the X-band transmitter never came back to life. This was not a stopper for the recovery of science data. The S-band transmitter used for command and telemetry could be used to stream the science data if at a slower rate, but the heat generated by the X-band transmitter was used to help keep the hydrazine fuel lines from freezing. With its power ebbing, its heaters off, and the X-band transmitter broken, Ulysses was destined to freeze and begin to tumble. Once it tumbles and loses lock on the Earth, recovery is impossible. It was determined that July 1st, 2008 would be the day that Ulysses was put to rest.
Since 1999, I’ve been working with the energetic particle data from the MF Spectrum Analyzer (MFSA) of the Heliosphere Instrument for Spectra, Composition and Anisotropies at Low Energy (HISCALE). Here the term “low energy” is relative. The HISCALE instrument measured protons and ions with energies from around 50 keV/nuc to upwards of 20 MeV/nuc and electrons from about 40 to 400 keV. The MFSA worked within the energy range of 50 to 5000 keV/nuc for protons, but provided a higher degree of energy resolution than anything else out there. Even though the spacecraft is now silent and adrift, we still have one and a half solar cycles worth of high-quality data that can yield a LOT of science.

Our immediate project at Fundamental Technologies is to organize and describe the data we have in such a way that it can be easily shared through the Virtual Heliospheric Observatory. If you’d like to use the HISCALE data or are just curious as to what we do at FunTech, browse over to http://ulysses.ftecs.com/ where I keep a blog on the current state of a few of our projects.