PDS_VERSION_ID = PDS3 RECORD_TYPE = STREAM LABEL_REVISION_NOTE = "2007-07-11 GEO:JGW; 2010-04-06 GEO:JGW, updated; 2011-04-19 Campbell, updates from peer review." OBJECT = INSTRUMENT INSTRUMENT_ID = "RTLS" INSTRUMENT_HOST_ID = "ARCB" OBJECT = INSTRUMENT_INFORMATION INSTRUMENT_NAME = "RADIO TELESCOPE" INSTRUMENT_TYPE = RADAR INSTRUMENT_DESC = " Instrument Overview =================== The following information comes from the NAIC website (http://www.naic.edu/public/the_telescope.htm): The radio telescope at Arecibo Observatory, located in Arecibo, Puerto Rico, is '305 m (1000 feet) in diameter, 167 feet deep, and covers an area of about twenty acres. The surface is made of almost 40,000 perforated aluminum panels, each measuring about 3 feet by 6 feet, supported by a network of steel cables strung across the underlying karst sinkhole. It is a spherical (not parabolic) reflector. Suspended 450 feet above the reflector is the 900 ton platform. Similar in design to a bridge, it hangs in midair on eighteen cables, which are strung from three reinforced concrete towers. One is 365 feet high, and the other two are 265 feet high. All three tops are at the same elevation. The combined volume of reinforced concrete in all three towers is 9,100 cubic yards. Each tower is back-guyed to ground anchors with seven 3.25 inch diameter steel bridge cables. Another system of three pairs of cables runs from each corner of the platform to large concrete blocks under the reflector. They are attached to giant jackswhich allow adjustment of the height of each corner with millimeter precision. Just below the triangular frame of the upper platform is a circular track on which the azimuth arm turns. The azimuth arm is a bow shaped structure 328 feet long. The curved part of the arm is another track, on which a carriage house on one side and the gregorian dome (installed in 1996) on the other side can be positioned anywhere up to twenty degrees from the vertical. Inside the gregorian dome two subreflectors (secondary and tertiary) focus radiation to a point in space where a set of horn antennae can be positioned to gather it.' The radar observations incorporated in this archive were produced by transmitting a circular-polarized radio signal at 2380 MHz frequency (12.6-cm wavelength) from the Arecibo Planetary Radar System. The typical transmit power was 45-100 kilowatts. Circular polarization is routinely used in planetary radar observations to avoid the complicating effects of Faraday rotation in the Earth's ionosphere. See 'An Astronomer's Guide to the Arecibo 305-m Telescope' [SALTER2009] for more information. " END_OBJECT = INSTRUMENT_INFORMATION OBJECT = INSTRUMENT_REFERENCE_INFO REFERENCE_KEY_ID = "SALTER2009" END_OBJECT = INSTRUMENT_REFERENCE_INFO END_OBJECT = INSTRUMENT END