Microwave Band Doppler Tracking of Spacecraft Observations in the low-frequency (LF, ~0.0001-0.1 Hz) spectral band require space-based detectors.
Laser interferometers in space, such as LISA, will fly by 2010
and promise very high sensitivity. However, the only current broadband technique in the LF
band uses the Earth and a distant spacecraft as free test masses in a "one-armed" interferometer,
coherence being maintained through a high-precision frequency standard on the ground. In this
technique, the Doppler tracking system of the NASA/JPL Deep Space Network (DSN), referenced to an
ultra-high-quality frequency standard, transmits a microwave tone to a distant spacecraft. The
signal is received at the spacecraft and phase-coherently retransmitted back to the earth.
The DSN antenna receives this transponded signal and compares its frequency with that of the
transmitted signal. The tracking system thus continuously measures the relative dimensionless
velocity (2 Dv/c ~ Df/fo) between the Earth and spacecraft. Unlike other GW detectors, the ~1-10 AU
Earth-spacecraft separation makes the Doppler detector large compared with the wavelength for most
candidate signals. In this regime, a GW incident on the Earth-spacecraft system is resolved into three
events in the Doppler time series: buffeting of the Earth, buffeting of the spacecraft, and the
initial buffeting of the Earth transponded back to the tracking station. These perturbations are of
order h, the GW strain amplitude, in Df/fo (see line drawing below). |
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Contact: John W. Armstrong john.w.armstrong@jpl.nasa.gov |
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send comments about this website to veronica@ligo.caltech.edu © California Institute of Technology updated on 7.2.2001 |
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