PDS_VERSION_ID = PDS3 LABEL_REVISION_NOTE = " 2012-08-30, D. Kazden, updated to meet PDS 3.8 standards; 2020-02-11, D. Kazden, updated cITATION_DESC;" OBJECT = DATA_SET DATA_SET_ID = "PVO-V-OETP-5-BOWSHOCKLOCATION-V1.0" OBJECT = DATA_SET_INFORMATION DATA_SET_NAME = "PVO VENUS ELECT TEMP PROBE DERVD BOW SHOCK LOCATION VER 1.0" DATA_SET_COLLECTION_MEMBER_FLG = N START_TIME = 1978-12-05T15:07:34.817 STOP_TIME = 1992-10-06T20:38:35.000 DATA_OBJECT_TYPE = TABLE ARCHIVE_STATUS = ARCHIVED DATA_SET_RELEASE_DATE = 1993-10-01 PRODUCER_FULL_NAME = "DR. ROBERT F. THEIS" DETAILED_CATALOG_FLAG = N ABSTRACT_DESC = "The Bow Shock File. This file gives the orbit-by-orbit times and locations of the bow shock crossings, which are characterized by distinct changes in Ne. Multiple shock crossing are listed if they are sufficiently separated to be resolved accurately. (Bow shock crossings will be evident in the High Resolution Ne File when they occurred within 30 minutes of periapsis)" DATA_SET_TERSE_DESC = "PVO VENUS ELECT TEMP PROBE DERVD BOW SHOCK LOCATION VER 1.0" CITATION_DESC = "Theis, R. F., PVO-V-OETP-5-BOWSHOCKLOCATION-V1.0, PVO VENUS ELECT TEMP PROBE DERVD BOW SHOCK LOCATION VER 1.0, NASA Planetary Data System, 1993." DATA_SET_DESC = " The Bow Shock File. This file gives the orbit-by-orbit times and locations of the bow shock crossings, which are characterized by distinct changes in Ne. Multiple shock crossing are listed if they are sufficiently separated to be resolved accurately. (Bow shock crossings will be evident in the High Resolution Ne File when they occurred within 30 minutes of periapsis). The ionopause and bow shock crossing times and locations are easily identified in the high resolution Ne measurements (Theis et al., 1980). These files contain the UT, altitude, latitude, SZA and local time of each crossing. The bow shock is a much more discrete feature in the data than the ionopause. Multiple shock crossings sometimes occur because the shock often moves at higher velocities than the satellite. In these cases, only the outer most shock crossing is recorded, unless the separation between the crossings is greater than a minute or two. The occurrence of multiple shocks in the Bow Shock File provides a record of the orbits in which the solar wind itself was probably highly variable. Because of the geometry of the orbit, most shock crossings were in the range of 45 to 135 deg. SZA. However, the nose region of the shock was explored between 1985 and 1987 when PVO periapsis was near the equator and was at altitudes between 2000 and 2300 km. During these years near solar minimum the nose of the shock often moved down into that altitude range (Russell et al, 1988). During the subsolar passages of these years, the orbit approximately paralleled the shock, sometimes inside, sometimes outside, thus providing interesting snapshots of its movements." CONFIDENCE_LEVEL_NOTE = " The bow shock is selected from 200 minute pass plots by marking the UT of the sharp change in the amplitude of Ne at the shock discontinuity. The resolution of the shock crossing time is of the order of 1 minute on these plots, but this could be improved to a few seconds if expanded plots were used. There is no plan currently to provide the ultimate resolution available in bow shock crossing time and location." END_OBJECT = DATA_SET_INFORMATION OBJECT = DATA_SET_MISSION MISSION_NAME = "PIONEER VENUS" END_OBJECT = DATA_SET_MISSION OBJECT = DATA_SET_TARGET TARGET_NAME = VENUS END_OBJECT = DATA_SET_TARGET OBJECT = DATA_SET_HOST INSTRUMENT_HOST_ID = PVO INSTRUMENT_ID = ONMS END_OBJECT = DATA_SET_HOST OBJECT = DATA_SET_REFERENCE_INFORMATION REFERENCE_KEY_ID = "RUSSELLETAL1988" END_OBJECT = DATA_SET_REFERENCE_INFORMATION OBJECT = DATA_SET_REFERENCE_INFORMATION REFERENCE_KEY_ID = "THEISETAL1980" END_OBJECT = DATA_SET_REFERENCE_INFORMATION END_OBJECT = DATA_SET END