PDS_VERSION_ID = PDS3 RECORD_TYPE = STREAM STANDARD_DATA_PRODUCT_ID = HEA DATA_SET_ID = "MEX-M-MRS-1/2/3-EXT2-3213-V1.0" PRODUCT_ID = "M00SUE0L1A_HEA_120380318_01.TXT" PRODUCT_CREATION_TIME = 2013-09-25T12:26:52.000 PRODUCER_ID = "SUE" INSTRUMENT_HOST_ID = "MEX" OBJECT = TEXT PUBLICATION_DATE = 2012-02-15 NOTE = "DSN MEX Bistatic Radar Data Report" END_OBJECT = TEXT END Miscellaneous ============= This is the first report since HEAC041A.TXT. Open Loop Data ============== Data Collection --------------- We have completed quick-look processing on the following MEX RSR open loop bistatic radar data at Stanford: DOY DSS RSR BAND RSR CH KSPS BT REC RECS RSR MAX START STOP ID RS LEN FILE NAME SNR --- --- -------- -------- ---- --- -- ---- -- ----- ----- ------------ ----- 038 14 05:46:00 06:08:00 -/XR 6 4 100 16 20260 26420 C038054E.RSR 35.2 038 14 05:46:00 06:08:00 -/SR 5 4 100 16 20260 26420 C038054F.RSR 22.6 038 14 05:46:00 06:08:00 -/XL 4 4 100 16 20260 26420 C038054G.RSR 29.2 038 14 05:46:00 06:08:00 -/SL 3 4 100 16 20260 26420 C038054H.RSR 14.9 038 14 06:08:00 06:30:00 -/XR 6 4 100 16 20260 26420 C038060A.RSR 44.6 038 14 06:08:00 06:30:00 -/SR 5 4 100 16 20260 26420 C038060B.RSR 29.5 038 14 06:08:00 06:30:00 -/XL 4 4 100 16 20260 26420 C038060C.RSR 42.4 038 14 06:08:00 06:30:00 -/SL 3 4 100 16 20260 26420 C038060D.RSR 29.1 038 14 06:30:00 06:52:00 -/XR 6 4 100 16 20260 26420 C038063A.RSR 31.7 038 14 06:30:00 06:52:00 -/SR 5 4 100 16 20260 26420 C038063B.RSR 22.3 038 14 06:30:00 06:52:00 -/XL 4 4 100 16 20260 26420 C038063C.RSR 30.5 038 14 06:30:00 06:52:00 -/SL 3 4 100 16 20260 26420 C038063D.RSR 17.8 038 14 06:52:00 07:14:00 -/XR 6 4 100 16 20260 26420 C038065A.RSR 20.8 038 14 06:52:00 07:13:59 -/SR 5 4 100 16 20260 26400 C038065B.RSR 9.8 038 14 06:52:00 07:14:00 -/XL 4 4 100 16 20260 26420 C038065C.RSR 26.3 038 14 06:52:00 07:14:00 -/SL 3 4 100 16 20260 26420 C038065D.RSR 15.1 Like the data described in HEAC041A.TXT, the 100 kHz data appear to be of good quality. Because of the large changes in Doppler frequency during the observations, the 100 kHz files may be more suitable for science analysis. Calibrations will have to be carried out using the 25 kHz data, since the 100 kHz recordings only cover the surface observations. Anomalies --------- An interfering signal passes through the S-Band frequency window at 06:17+/-3 minutes. It should have relatively little impact on the analysis.