PDS_VERSION_ID = PDS3 RECORD_TYPE = STREAM OBJECT = TEXT NOTE = "Known errors and/or anomalies in the volumes" PUBLICATION_DATE = 2012-09-10 END_OBJECT = TEXT END ERRORS AND/OR ANOMALIES IN THE CURRENT VOLUME Volume CORADR_0231, Version 02 ------------------------------ 1. The Cassini Radar Transition file (EXTRAS/CRT_231_V02.TAB) contains no information about ScanStart and ScanEnd transitions. 2. In the volume index table (INDEX/INDEX.TAB), double quotes enclose all the date/time values. Normally, PDS date/time values are not quoted, but quoting makes parsing easier for some applications. 3. The HTML documents in the DOCUMENT directory contain HTML character codes that, while all-ASCII, are not easily interpretable by someone who is reading the HTML documents as text documents. For example, "α" represents the lower-case Greek character "alpha" and is rendered as such in a web browser. Equivalent and more legible character codes (e.g., "&#alpha;") are available as of the HTML 4.0 specification but cannot be used here, as PDS requires HTML documents to comply to the HTML 3.2 specification. 4. Antenna temperature, brightness temperature, and receiver temperature are defined in Janssen, M. A., "An Introduction to the Passive Microwave Remote Sensing of Atmospheres," Chapter 1 in Atmospheric Remote Sensing by Microwave Radiometry, (M. Janssen, ed.), pp. 1-35, Wiley & Sons, New York (1993). The archived value in the SBDR and LBDR files gives uncalibrated antenna temperature in units of Kelvin. The best current algorithm for correcting the archived antenna temperatures is Ta_corrected = Ta_archive * ( 0.920 - 0.0041*( t - 1.90 ) ) where t = time in years and fractional years since 2004.0 (0 UTC on 1 Jan 2004) This algorithm is based on the radioastronomical flux scale at 2-cm wavelength by direct comparison of distant (unresolved) Titan measurements by the Cassini radiometer with VLA measurements of Titan reported by Butler and Gurwell, 2004. This algorithm will improve with time as more distant Titan measurements are obtained and as more radioastronomical comparison sources are included. Butler, B. J., Gurwell, M. A. 2004. Radio Wavelength Observations of Titan with the VLA. Bull. Am. Astron. Soc. 36, 6.04. This algorithm applies also to all preceeding volumes. 5. Ideally the calibrated antenna temperature is referenced to cold sky at 2.7 K, although no guarantee is made that this zero-level accounting has been correctly made. Also, the antenna temperature is defined for this application as just the average brightness temperature in the measured beam out to 2 degrees from the beam axis, and does not allow for possible contributions from the far sidelobes (sidelobes outside of 2 degreees). The archived value will include an additional contribution if the far sidelobes happen to fall on other than cold sky. In particular, there is an offset to be expected and accounted for when an extended source like Titan or Saturn is observed from a close distance. A more detailed explanation will be found in Janssen et al., 2009. System gain is the quantity that multiplies the raw sky counts to convert to the uncalibrated Kelvin scale. Receiver_temp is the receiver noise temperature Tr (comparison made at internal reference switch). The receiver temperature plus the antenna temperature is equal to the total signal (raw counts times system gain). 6. ant_temp_std is a measure of the rms uncertainty of Ta, and is only an estimation. It is obtained as the standard deviation of Ta for three points, Ta(I-1), Ta(I), and Ta(I+1), and is a useful measure that identifies questionable data. For example, it gets large when the beam is sweeping across a brightness discontinuity. 7.The submitted volume CORADR_0143 has an erroneous INDEX and CUMINDEX entry for BIFQE10N073_D143_I049S01_V02. 8.Every volume from CORADR_0144 to CORADR_0229 has missing CUMINDEX entries for Iapetus_049_3. ERRORS AND/OR ANOMALIES IN PREVIOUS VOLUMES Not Applicable