Kepler's Equation
Kepler's equation links time in an elliptical orbit to eccentric anomaly, making it a core tool for finding where an orbiting body is.
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Kepler's equation links time in an elliptical orbit to eccentric anomaly, making it a core tool for finding where an orbiting body is.
Eccentric anomaly is a geometric helper angle used to connect orbital time with an object's actual position on an elliptical orbit.
Mean anomaly is a time-based angle that tracks how far an orbiting body has progressed since periapsis in an ideal Keplerian orbit.
True anomaly is the angle that gives an orbiting object's actual position along an elliptical orbit relative to periapsis.
The argument of periapsis is the angle that locates an orbit's closest point within its own orbital plane.
Apsidal precession is the slow rotation of an orbit's closest and farthest points, changing where periapsis and apoapsis occur.
Nodal precession is the slow rotation of an orbit's line of nodes, changing where a tilted orbit crosses its reference plane.
The ascending node is the point where an orbiting object crosses a reference plane moving northward, anchoring an orbit's orientation in space.
Orbital inclination measures the tilt of an orbit against a chosen reference plane, helping define where an object travels through space.
Orbital eccentricity measures how much an orbit departs from a circle, shaping distances, speeds, and sunlight patterns along a path.
Milankovitch cycles are slow changes in Earth's orbit and orientation that alter sunlight patterns and help pace ice-age climate cycles.
Axial tilt is the angle between a planet's rotation axis and its orbital plane, and on Earth it drives the pattern of seasons.
A solstice is one of the two yearly moments when the Sun reaches its greatest north or south position in the sky.
An equinox is one of the two moments each year when the Sun crosses the celestial equator, marking a seasonal turning point.
The ecliptic is the Sun's apparent yearly path on the celestial sphere and the projection of Earth's orbital plane.
The celestial sphere is an imaginary sky sphere that helps astronomers describe positions and motion in the night sky.
Declination is the north-south coordinate astronomers use to locate objects above or below the celestial equator.
Hour angle is an astronomy coordinate that tells how far a celestial object is from crossing an observer's meridian.
Right ascension is the sky-coordinate measure astronomers use to locate objects eastward around the celestial equator.
Sidereal time is an astronomical way of keeping time by Earth's rotation relative to the stars rather than the Sun.
International Atomic Time, or TAI, is the continuous atomic time scale that underpins UTC, scientific timing, navigation, and modern time standards.
A leap second is a one-second adjustment to Coordinated Universal Time, used to keep civil time close to Earth's uneven rotation.
Coordinated Universal Time, or UTC, is the international reference time scale used to synchronize civil time, networks, navigation, science, and time zones around the world.
Remote sensing is the science of collecting information about objects or places from a distance, usually with sensors on satellites, aircraft, drones, or ground platforms.