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6.1 Observations to date

Table 3 lists spacecraft Doppler GW observations to date.


Table 3: Spacecraft Doppler Gravitational Wave Observations. MO: Mars Observer; GLL: Galileo; ULS: Ulysses; MGS: Mars Global Surveyor; AMC: Advanced Media Calibration system (tropospheric calibration). A “pass” is a tracking pass over a given DSN antenna, i.e. about 8 hours long.








Year Spacecraft

Comment

Reference




       
1980 Voyager

several passes; S-band uplink, S/X downlink; burst search

[57Jump To The Next Citation Point]
1981 Pioneer 10

3 passes; long T2; GW background limit; observationally excluded GW from Geminga

[4Jump To The Next Citation Point6Jump To The Next Citation Point]
1983 Pioneer 11

3 days; long T2; broadband periodic search

[18Jump To The Next Citation Point]
1988 Pioneer 10

10 days; long T2; chirp wave search

[5]
1990 Ulysses

3.5 days; short T2

[26Jump To The Next Citation Point25Jump To The Next Citation Point]
1992 Ulysses

14 days; long T2; periodic and chirp search; S-band uplink, S/X band downlink

[26Jump To The Next Citation Point25Jump To The Next Citation Point]
1993 MO/GLL/ULS

19 days; X/X-band on MO; coincidence experiment; search for all waveforms

[60Jump To The Next Citation Point61Jump To The Next Citation Point13Jump To The Next Citation Point]
1994-5 Galileo

40/40 days (two oppositions); long T2; S/S-band

[3Jump To The Next Citation Point13Jump To The Next Citation Point]
1997 MGS

21 days; short T2; X/X-band

[9Jump To The Next Citation Point]
2001-3 Cassini

40/40/20 days (three oppositions); long T2; Ka-band; AMC; multi-link plasma calibration

[19Jump To The Next Citation Point74]








       

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 10View Image) 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 [57Jump To The Next Citation Point]. 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 [4Jump To The Next Citation Point] and place the then-best limit on a low-frequency GW background [6Jump To The Next Citation Point]. 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 [2625Jump To The Next Citation Point]. 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 [60Jump To The Next Citation Point13Jump To The Next Citation Point] 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) [9Jump To The Next Citation Point]. 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 [9Jump To The Next Citation Point22].

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 [641145930113]) and by the Advanced Media Calibration system (allowing excellent tropospheric scintillation removal) [889019Jump To The Next Citation Point72].


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