RADAR Engineering Technical Write-up
TL: Dr. Charles Elachi
RADAR General Description:
The Cassini Radar (RADAR) uses the five-beam Ku-band antenna feed
assembly associated with the spacecraft high gain antenna to direct
radar transmissions toward targets, and to capture blackbody radiation
and reflected radar signals from targets.
RADAR Scientific Objectives:
- To determine whether oceans exist on Titan, and, if so, to determine their distribution.
- To investigate the geologic features and topography of the solid surface of Titan.
- To acquire data on non-Titan targets (rings, icy satellites) as conditions permit.
RADAR Sensing Instruments:
- Synthetic Aperture Radar Imager [SAR] (13.78 GHz Ku-band; 0.35 to 1.7 km resolution)
- Altimeter (13.78 GHz Ku-band; 24 to 27 km horizontal, 90 to 150 m vertical resolution)
- Radiometer (13.78 GHz passive Ku-band; 7 to 310 km resolution)
RADAR Instrument Characteristics:
- Mass (current best estimate) = 41.43 kg
- Peak Operating Power (current best estimate) = 108.40 W
- Peak Data Rate (current best estimate) = 364.800 kilobits/sec
The Cassini Radar (RADAR) will be used to investigate the surface of
Saturn's moon Titan by taking four types of observations: imaging,
altimetry, backscatter, and radiometry. In the imaging mode of operation,
the RADAR instrument will bounce pulses of microwave energy off the
surface of Titan from different incidence angles and record the time it
takes the pulses to return to the spacecraft. These measurements, when
converted to distances (by dividing by the speed of light), will allow
the construction of visual images of the target surface. Radar will be
used to image Titan because the moon's surface is hidden from optical
view by a thick, cloud-infested atmosphere: radar can "see" through
such cloud cover.
Radar altimetry similarly involves bouncing microwave pulses off the
surface of the target body and measuring the time it takes the "echo"
to return to the spacecraft. In this case, however, the goal will not
be to create visual images but rather to obtain numerical data on the
precise altitude of the surface features of Titan. In the backscatter
mode of operation, the RADAR will act as a scatterometer. That is, it
will bounce pulses off Titan's surface and then measure the intensity
of the energy returning. This returning energy or backscatter, is
always less than the original pulse, because surface features
inevitably reflect the pulse in more than one direction. From the
backscatter measurements, scientists can infer the composition of the
surface of Titan.
Finally, in the radiometry mode, the RADAR will operate as a passive
instrument, simply recording the energy emanating from the surface of
Titan. This information will tell scientists the amount of latent heat
(i.e.. moisture) in the moon's atmosphere, a factor that has an impact
on the precision of the other measurements taken by the instrument.
During imaging, altimetry, and backscatter operations, the RADAR
instrument will transmit linear frequency-modulated Ku-band pulsed
signals toward the surface of Titan using the high-gain antenna (HGA).
These signals, after reflection from the surface, will be captured by
the same antenna and detected by the RADAR Radio Frequency Electronics
Subsystem. During radiometry operations, the instrument will not
transmit any radar signals, but the HGA will again be used for
radiometric observations.
To improve the surface coverage by radar imaging, a switched, multiple
Ku-band antenna feed array structure is part of the HGA and permits the
formation of five antenna beam patterns. Each of these beams will have
a different pointing angle relative to the antenna reflector's focal
axis.
The major functional components of the RADAR Subsystem are the Radio
Frequency Electronics Subsystem, the Digital Subsystem, and the Energy
Storage Subsystem. For information on these components, click on their
names.