Scientists have measured temperatures beneath the surface of Jupiter’s volcanic moon Io, offering the first-ever glimpse of the hidden heat driving the most volcanically active world in the solar system.
During close flybys of Io in late 2023 and early 2024, NASA’s Juno spacecraft turned its Microwave Radiometer (MWR) instrument toward the moon, probing roughly six to 20 feet (two to six meters) beneath its surface. Originally designed to peer through Jupiter’s thick clouds, the instrument instead revealed a powerful new way to study how heat moves through planetary crusts, according to a statement from the space agency.
“The surprising discovery that we could see below a rocky moon’s surface has important implications for studying Earth’s volcanoes,” Scott Bolton, coauthor of the study and Juno’s principal investigator, said in the statement. “Juno has taught us that if we look with an MWR-type instrument near a volcano on Earth, we might see a similar signature in the subsurface temperature gradient, providing new information on how terrestrial volcanoes work.”
Until now, researchers had relied almost entirely on infrared observations, which detect only the temperature of Io’s surface. By probing several feet underground, Juno has revealed how heat moves through the moon’s crust for the first time.
The measurements showed temperatures rising by more than 40 degrees Fahrenheit (22 degrees Celsius) just a few feet below the surface — far more than sunlight alone could explain. Juno’s subsurface heat map also revealed localized regions of elevated heat, with temperatures measuring between 18 and 36 degrees F (10 to 20 degrees C) warmer than the surrounding terrain, according to the statement.
Juno’s observations uncovered another surprise, too. Despite being known for its towering mountains and active volcanoes, much of Io’s surface appears remarkably smooth and composed of unusually low-density material. Researchers think the moon is blanketed by porous layers of volcanic ash, sulfur frost and other eruptive debris that continually resurface Io, burying older terrain beneath fresh deposits.
Scientists think the heat detected beneath Io’s surface could be rising steadily from the moon’s molten interior through a conductive crust or coming from pockets of cooling lava flows trapped just below the surface. Either way, the data provide the clearest picture yet of how Io transports heat from its interior.
Unlike Earth, where volcanism is driven largely by heat from radioactive decay, Io is continuously stretched and squeezed by Jupiter’s immense gravity as it orbits the giant planet. This constant tidal flexing generates enormous amounts of internal heat, fueling hundreds of active volcanoes and making Io the most volcanically active object in the solar system. By improving scientists’ understanding of how heat and magma move beneath a planet’s surface before eruptions, the same microwave techniques used by Juno could one day help researchers better monitor Earth’s volcanoes and improve eruption forecasting.
“Io provides a unique window into learning how tidal heating works throughout the cosmos, a fundamental process that provides energy and heat to worlds that are far from their parent star,” Bolton said in the statement. “This process can not only create the most volcanic body in the solar system, in the case of Io, but also fuels the subsurface oceans on the moons of giant planets, such as Europa and Ganymede. Up until this point we could only observe the heat escaping at the surface or through eruptions. Now we can characterize how the heat is moving from the interior toward the surface.”
Because Io is an extreme example of volcanic activity, it serves as a natural laboratory for studying how heat moves through planetary crusts. Those insights could help scientists better understand ancient volcanism on Mars, Venus, and Earth’s moon, whose landscapes were shaped by massive eruptions billions of years ago.
The technique could also aid the search for life elsewhere. While Io itself is far too hostile to support life, microwave instruments can also probe beneath icy surfaces. Juno has already used the same instrument to study Jupiter’s moons Europa and Ganymede, where scientists believe vast oceans lie hidden beneath thick shells of ice. Understanding how heat moves through those crusts is key to determining whether they could harbor environments suitable for life as we know it.
Their findings were published July 22 in the Journal of Geophysical Research: Planets.
