Planet: Apparent Cartesian Velocity

The apparent velocity of the planet, expressed in Cartesian components, as a function of time. The apparent velocity is computed with respect to the scenario's central body as observed in the requested frame. The apparent position can be requested in a variety of coordinate systems. The available coordinate systems depend on the scenario's central body. Nominally, the systems Fixed, Inertial, J2000, TrueOfDate, and MeanOfDate are supported, although some central bodies (notably the Earth and Sun) have more. The following lists the systems available for Earth.

Type: Time-varying data

Availability: Reports | Graphs | Dynamic Displays | Strip Charts

NameDescription
FixedA coordinate system attached to the central body and rotating with it.
ICRFEarth's attitude expressed with respect to the ICRF frame.
MeanOfDateThe mean equator mean equinox coordinate system evaluated at the requested time.
MeanOfEpochThe mean equator mean equinox coordinate system evaluated at the epoch of the object.
TrueOfDateThe true equator true equinox coordinate system evaluated at the requested time.
TrueOfEpochThe true equator true equinox coordinate system evaluated at the epoch of the object.
B1950 The mean equator mean equinox coordinate system evaluated at the beginning of the Besselian year 1950 (31 December 1949 22:09:46.866 = JD 2433282.4234591).
TEMEOfEpochThe true equator mean equinox coordinate system evaluated at the epoch of the object.
TEMEOfDateThe true equator mean equinox coordinate system evaluated at the requested time.
AlignmentAtEpochThe non-rotating coordinate system coincident with the Fixed system evaluated at the object's coordinate reference epoch.
J2000 The mean equator mean equinox coordinate system evaluated at the J2000.0 epoch (2000 January 1.5 = JD 2451545.0 TDB).