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-IONOPAUSELOCATION-V1.0" OBJECT = DATA_SET_INFORMATION DATA_SET_NAME = "PVO VENUS ELECT TEMP PROBE DERVD IONOPAUSE LOCATION VER 1.0" DATA_SET_COLLECTION_MEMBER_FLG = N START_TIME = 1978-12-05T15:07:34.817 STOP_TIME = 1992-10-07T19:46:27.000 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 Ionopause File. This file gives the orbit-by-orbit times and locations of the ionopause crossings, which are evident as sharp gradients in Ne at the top of the ionosphere. (These crossings always occur within 30 minutes of periapsis, so they may be seen in the High Resolution Ne files)." DATA_SET_TERSE_DESC = "PVO VENUS ELECT TEMP PROBE DERVD IONOPAUSE LOCATION VER 1.0" CITATION_DESC = "Theis, R. F., PVO-V-OETP-5-IONOPAUSELOCATION-V1.0, PVO VENUS ELECT TEMP PROBE DERVD IONOPAUSE LOCATION VER 1.0, NASA Planetary Data System, 1993." DATA_SET_DESC = " The Ionopause File. This file gives the orbit-by-orbit times and locations of the ionopause crossings, which are evident as sharp gradients in Ne at the top of the ionosphere. (These crossings always occur within 30 minutes of periapsis, so they may be seen in the High Resolution Ne files). 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. On the dayside, the ionopause is taken (somewhat arbitrarily) at the level in the steep gradient of the ionopause where Ne = 1x102 cm-3. On the nightside, the ionopause is selected at somewhat lower densities because the absence of spacecraft photoelectrons lowers the Ne measurement threshold. In both cases, the intent is to identify the ionopause as the point where the first rise of Ne above the background density occurs. Of course, the ionopause itself is not a point but is the extend region in which the ionopause density gradient occurs." CONFIDENCE_LEVEL_NOTE = " The ionopause location is selected at that point in the steep gradient of the ionopause where Ne crosses through the level of 1x102 cm-3. When the spacecraft is in darkness, the pe background is absent and the ionospheric Ne is also much lower, so the ionopause is identified as the first rise in Ne above whatever background is present. The ionopause is identified by a human operator who views each high resolution Ne pass plot on an interactive computer terminal. He selects the ionopause somewhat subjectively as the time of the first rise above the background Ne, which may consist of magnetosheath plasma or photoelectrons. The 40 minute pass plots used for this purpose provide only a 5-10 second accuracy in the crossing times. When irregularities or waviness in the ionopause produce several ionopause crossings, the outer most crossing is the only one identified." 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 = "THEISETAL1980" END_OBJECT = DATA_SET_REFERENCE_INFORMATION END_OBJECT = DATA_SET END