PDS_VERSION_ID = PDS3 LABEL_REVISION_NOTE = "2001-07-19 CU:BTCarcich" /* File Characteristics */ RECORD_TYPE = FIXED_LENGTH RECORD_BYTES = 50 FILE_RECORDS = 16471 /* Data Object Pointers */ ^TABLE = "EROSRGST_2001012.TAB" /* Identification Keywords */ DATA_SET_ID = "NEAR-A-MSI-5-EROS-SHAPE-MODELS-V1.0" PRODUCT_NAME = "433 EROS SHAPE MODEL" PRODUCT_ID = "RGST-EROS-2001012" INSTRUMENT_HOST_NAME = "NEAR EARTH ASTEROID RENDEZVOUS" INSTRUMENT_NAME = "MULTI-SPECTRAL IMAGER" TARGET_NAME = EROS START_TIME = "N/A" STOP_TIME = "N/A" PRODUCT_CREATION_TIME = 2001-01-12 /* Model Creation Date */ RECORD_FORMAT = "(f8.1,f8.1,f8.2,f8.3,f8.2,f8.2)" /* Data Object Descriptions */ OBJECT = TABLE ROWS = 16471 ROW_BYTES = 50 INTERCHANGE_FORMAT = ASCII COLUMNS = 6 DESCRIPTION = "Numerical model of 433 Eros, derived solely from NEAR-SHOEMAKER data. This model comprises a grid with points every two degrees in latitude and west longitude, and four data associated with each point. The model is written with both 0 and 360 longitude entries. Coordinates are planetocentric. N.B. In this RGST-EROS-2001012 product, some radii starting from the model center intersect the surface in more than one point. This happens mostly around 160 degrees west longitude. That means that the RGST format used in this product is not able to adequately represent the shape model's surface. Caveat emptor. If this is an issue, users may use one of the plate models. See the catalog file, erossmds.cat, for this data set. See Thomas, et al. (2001) [THOMASETAL2001] for details of this shape model." OBJECT = COLUMN COLUMN_NUMBER = 1 NAME = "LATITUDE" UNIT = DEGREE DATA_TYPE = ASCII_REAL START_BYTE = 1 BYTES = 8 FORMAT = "F8.1" END_OBJECT = COLUMN OBJECT = COLUMN COLUMN_NUMBER = 2 NAME = "LONGITUDE" UNIT = DEGREE DATA_TYPE = ASCII_REAL START_BYTE = 9 BYTES = 8 FORMAT = "F8.1" END_OBJECT = COLUMN OBJECT = COLUMN COLUMN_NUMBER = 3 NAME = "RADIUS" DESCRIPTION = "Model radius for this latitude and longitude. This is the distance of the surface grid point from the center of the model." UNIT = KILOMETER DATA_TYPE = ASCII_REAL START_BYTE = 17 BYTES = 8 FORMAT = "F8.2" END_OBJECT = COLUMN OBJECT = COLUMN COLUMN_NUMBER = 4 NAME = "ACCELERATION" DESCRIPTION = "Model gravity for this latitude and longitude. This is the magnitude of the acceleration, in cm/s/s, due to local gravity at the grid point, including the effect of Eros' rotation. The direction of the gravity vector is not specified." UNIT = "CM/S/S" DATA_TYPE = ASCII_REAL START_BYTE = 25 BYTES = 8 FORMAT = "F8.3" END_OBJECT = COLUMN OBJECT = COLUMN COLUMN_NUMBER = 5 NAME = "SLOPE" DESCRIPTION = "Model slope for this latitude and longitude. This is the local slope, in degrees, of the surface relative to an equipotential surface at the grid point. In other words, it is the angle between the local gravity vector and the local surface normal. The local gravity vector includes the effect of Eros' rotation." UNIT = DEGREE DATA_TYPE = ASCII_REAL START_BYTE = 33 BYTES = 8 FORMAT = "F8.2" END_OBJECT = COLUMN OBJECT = COLUMN COLUMN_NUMBER = 6 NAME = "TOPO HEIGHT" DESCRIPTION = "Model topography for this latitude and longitude. This is the local potential energy of the surface at this grid point relative to the surface at the south pole, divided by the mean surface gravitational acceleration for Eros of .47 cm/s/s. The result is a rough analog to topographic height or elevation. The local gravity vector used to calculate this datum includes the effect of Eros' rotation." UNIT = KILOMETER DATA_TYPE = ASCII_REAL START_BYTE = 41 BYTES = 8 FORMAT = "F8.2" END_OBJECT = COLUMN END_OBJECT = TABLE END