A unit of length equal to the radius of the Earth, used to describe the size of exoplanets.Earth radius is a standard unit of length equal to the mean radius of our planet, approximately 6,371 kilometers. In astronomy, it is commonly used to describe the sizes of exoplanets, especially rocky worlds and super-Earths, providing a familiar reference point for comparing distant planets to our own. When astronomers measure the transit depth of a planet passing in front of its star, they derive its radius in Earth units, which helps classify it as terrestrial, Neptune-like, or gas giant.
The concept of Earth's radius dates back to ancient Greek measurements by Eratosthenes around 240 BCE, who estimated it within a few percent of the modern value. Its use as a unit for exoplanets became standard with the discovery of the first transiting exoplanets in the early 2000s.
The Earth radius is defined as the average distance from the planet's center to its surface, accounting for the equatorial bulge and polar flattening. For exoplanets, the radius is typically measured via the transit method: the fraction of starlight blocked during a transit equals the square of the planet's radius divided by the star's radius. By combining this with the star's known size, astronomers express the planet's radius in Earth radii, enabling comparisons of planetary compositions and structures.
Earth radius is used to categorize exoplanets, such as distinguishing super-Earths (1–2 Earth radii) from mini-Neptunes (2–4 Earth radii), which informs models of planetary formation and habitability.
The first exoplanet with a measured radius in Earth units was HD 209458b, a hot Jupiter with a radius about 1.4 times that of Jupiter, not Earth, but the unit quickly became standard for all exoplanets.























