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Early Webb analyses put giant planet HATS-6 b about 300 degrees Celsius below its standard estimate
University of Maryland astronomers using Webb found ammonia on HATS-6 b and early temperatures near 120 C, against the 425 C usually cited. Their leading suspect is reflective cloud, and the planet's chemistry readings depend on that temperature.
The Scientist · Science desk

What happened
- A University of Maryland-led team used Webb to find water, methane, ammonia and carbon dioxide in the atmosphere of HATS-6 b, publishing in the Astronomical Journal.
- HATS-6 b is roughly the size of Jupiter and circles a small, cool M-dwarf star once every three days, 500 light-years from Earth.
- The ammonia is only the second time transmission spectroscopy, which reads starlight filtering through an atmosphere, has found that molecule on a distant world.
- Early analyses put the planet's temperature near 120 C, well below the roughly 425 C figure usually cited for it.
- HATS-6 b is one of seven planets in Webb's GEMS program, drawn from about 40 known giant planets orbiting M dwarfs.
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Why it matters
- exposure Temperature enters every calculation of what an atmosphere contains, so a gap of about 305 degrees would carry into composition readings for other planets around small, active stars.
- contradiction The same report calls a 120 C reading physically improbable for a three-day orbit, so the cold result is provisional even as the team weighs clouds to explain it.
- capability Ammonia gives GEMS a nitrogen tracer for testing whether giants around M dwarfs are a chemically separate population from hot Jupiters around sun-like stars.
Nobody ever measured the 425 C figure usually attached to HATS-6 b. It is a shortcut with two built-in assumptions: the planet absorbs all the light its star delivers, and it spreads that heat evenly [11]. The early Webb analyses came in about 305 degrees below it [1].
Giannina Guzmán Caloca, the study's lead author and an astronomy Ph.D. candidate at the University of Maryland, goes after the first assumption. "If the planet is genuinely that cool, it means that something is probably reflecting a great deal of starlight back into space before it can warm anything," she said. "The likeliest explanation is cloud and haze wrapping the planet the way they wrap Venus." [14] If clouds are the answer, the physics of stellar heating holds, and what fails is the assumption that the planet reflects nothing.
Formation is the older and firmer puzzle. Planets build from the disk of gas and dust left around a young star, and smaller stars have smaller disks [4]. "These smaller stars don't have enough material or enough time to create planets as big as Jupiter and as big as Saturn," Guzmán Caloca said. "So, the fact that HATS-6 b can exist is really interesting because it shouldn't be possible with what we know." [5]
The sample is small. GEMS covers roughly one in six of the known giants around M dwarfs [2]. The whole class is under 1 percent of the more than 6,000 exoplanets found so far [17][3]. The program's comparison group is the better-understood giants around sun-like stars [6]. "By measuring what their atmospheres are made of, we can start to ask whether they were built the same way as the hot Jupiters around sun-like stars or whether something different is going on," she said [7].
Ammonia is the chemical clue in this result. Nitrogen-bearing molecules should be more abundant in cooler giant planets than in scorching ones [9], so finding ammonia fits a planet on the cold side of the estimate. "Carbon, hydrogen and oxygen are all things that have previously been found in atmospheres of giant planets outside our solar system, but ammonia is something almost never detected before," Guzmán Caloca said. "It's an entirely new molecule to think about." [8]
The thing this doesn't tell you is how HATS-6 b formed. The data cover one planet out of seven [6], and its temperature comes from early analyses [12]. That is not yet enough to tell an unusual formation route apart from an unusually cloudy atmosphere. In my view the evidence backs the formation puzzle, which rests on the planet existing at all. It gives much weaker support to the idea that heating models fail, because the team's own leading explanation is reflective cloud [14].
What to watch
- Longer-wavelength observations, which the team says could test whether clouds explain the low temperature and identify other unexplained signals.
- Whether the other six GEMS planets also show ammonia, or temperatures that fall short of their standard estimates.
- Whether later analyses of HATS-6 b hold near 120 C or move back toward the 425 C estimate.