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The observations in Table 3 reflect increasing sensitivity between
1980 and the present. These
sensitivity improvements were due both to engineering improvements (in spacecraft and in the DSN) and to
programmatic decisions allowing use of planetary spacecraft for these observations. Voyager
sensitivity was limited by a combination of plasma noise in the S-band uplink (see Figure 10
)
and spacecraft buffeting noise from its thrusters. Although the data volume was small, those
observations were used in the first formal search for low-frequency burst waves [57
]. The Pioneer
spacecraft were spin-stabilized, resulting in lower spacecraft buffeting noise, but were again
sensitivity-limited by plasma noise in the S-band radio links. Despite this, Pioneer data were able to
observationally exclude putative sinusoidal GW emission from Geminga [4
] and place the then-best
limit on a low-frequency GW background [6
]. Ulysses observations in 1992 were the longest to
date, motivated innovations in signal processing, and resulted in the then-best sensitivity to
periodic and chirp waveforms [26, 25
]. Mars Observer was the first spacecraft to have X-band on
both the up- and downlinks, resulting in much-reduced plasma noise. Mars Observer, Galileo,
and Ulysses did the first (and so far only) coincidence experiment [60
, 13
] which was used
successfully to disqualify an event which was formally significant in one time series. Galileo
observations in 1994 – 1995 had a long two-way light time and thus better GW response at lower
Fourier frequencies. Unfortunately, the failure of the high-gain antenna required S-band only
observations (thus high plasma noise) [9
]. Mars Global Surveyor observations in 1997 were
done with X-band links (but off of solar opposition) and were the only observations where
spacecraft engineering telemetry was used to correct the Doppler data for the (slow) systematic
spacecraft motion. Those data also showed strong correlation at the two-way light time, indicating
the importance of tropospheric calibration and placing upper limits on antenna mechanical
noise [9
, 22].
Most of the sensitivity discussion in this paper, however, relates to Cassini observations. Cassini was
launched on a mission to Saturn in 1997 [68]. After earth, Venus, and Jupiter gravity-assists, it
continued on a free interplanetary cruise trajectory toward orbit insertion at Saturn. The Cassini
gravitational wave observations consisted of two 40-day data-taking campaigns, centered on the
spacecraft’s solar oppositions during 2001 – 2002 and 2002 – 2003, and one 20 day observation taken
somewhat off opposition during late 2003. This data set is distinguished by its very sophisticated
multi-link radio system (allowing essentially perfect plasma correction [64, 114, 59, 30, 113])
and by the Advanced Media Calibration system (allowing excellent tropospheric scintillation
removal) [88, 90, 19
, 72].
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