Icy Moon in Radio Waves ✎ express

Original: "Radar observations of Europa in 2011-2024: New insights into radar scattering properties"
arXiv:2608.17689v1 · 2026-08-18 · arXiv non-exclusive · independent analysis · 1 min
Radar peered beneath Europa's icy crust and saw how it reflects radio waves.

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From 1987 to 1991, astronomers last measured how Jupiter's icy moons reflect radio waves. Then came a long pause. In 2011–2024, researchers aimed a radar beam at Europa again: this time using the 70-meter antenna at Goldstone and the Green Bank Telescope.

Ice is nearly transparent to radio waves, like clear window glass is to light. By sending a signal and catching its reflection, you can learn what's happening in the upper tens of meters of the icy crust. The radar showed that Europa's leading side (the one facing forward in its orbit) reflects waves differently than the trailing side. It's as if one half of a mirror were frosted and the other polished.

The radio signal penetrates Europa's ice about 32 meters — roughly the height of a nine-story building.

Such a difference hints that the moon's surface is not uniform: in some places the ice is cleaner and denser, in others it's loose or mixed with impurities. Understanding these differences helps reconstruct Europa's history and assess how deep beneath the ice a liquid water ocean might hide.

Radio waves pass through clean ice for tens of meters, so radar sees Europa's subsurface layers the way ultrasound sees a baby in the womb.

In Arthur C. Clarke's novel "2010: Odyssey Two," Europa is depicted as a world that must not be touched, and radar observations allow us to study it without getting close.

Scientists
Michael FaradayHendrik LorentzCharles TownesRobert Woodrow WilsonRobert H. DickeKarl Jansky
Concepts
europa gaia telescope Planck satellite Satellite layers radar erosita gaia ixpe euclid virgo OISST v2.1 GPCP