Astronomers have drawn exoplanets as perfect circles for decades, neat silhouettes fringed by a uniform ring of atmosphere. That picture was always a convenience, and now it has been measured away. A team co-led by Cornell University in the United States and the University of Bristol in the United Kingdom has mapped the actual, lopsided contours of an exoplanet's atmosphere for the first time: a deformed sphere stretched and squeezed by ferocious winds, with a temperature contrast of roughly 650 kelvin between its morning and evening skies.
The target was WASP-17b, a hot Jupiter orbiting a star some 1,300 light-years from Earth. The study, published in Nature Astronomy, is the first application of a new analytical method called transmission strings, applied to data from the James Webb Space Telescope. It turns what had been an abstract prediction of atmospheric circulation into a measured structure, including a broad banded jet around the equator ferrying heat and material from the planet's permanent dayside toward its permanent night side.
The ring that was never real
When a planet crosses in front of its star, a sliver of starlight filters through the gas at the planet's edge, and molecules in that gas imprint telltale absorption signatures on the stellar spectrum. For years, the standard analysis treated the atmosphere visible during a transit as a single uniform ring. That approach can identify molecules, but it flattens a dynamic, three-dimensional atmosphere into one limb-averaged spectrum, blending together the morning and evening terminators, the equator and the poles.
The simplification mattered because the blending was assumed, not observed. Models of irradiated planets predict substantial horizontal temperature gradients that reshape both the scale height of the atmosphere and its chemistry from dayside to nightside and from equator to pole. Without a way to resolve those variations, theorists could only test their models against each other, never against a real, measured geometry.
Pulling strings
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Transmission strings, also called transit mapping, works in a fundamentally different way. Rather than assuming the atmosphere is a circle with the same radius all the way around, the method tracks the planet as it crosses the star, capturing the composition of starlight filtering around the limb from many different angles as the transit progresses. It then pulls out different distances from the center to the edge of the planet at each point along the rim.
The technique was developed at Bristol by astrophysicists Dr. David Grant and Dr. Hannah Wakeford. The new paper's lead author is Dr. Lili Alderson, a Klarman postdoctoral fellow at Cornell University who carried out the research as part of her doctoral work in physics at the University of Bristol. With JWST data, Alderson and her team measured the shape of the transmitting limb as a function of angle across the poles for the first time.
We have gone from a ring to understanding where on the ring the gemstones are, so to speak.
That is how Alderson describes what the technique achieves. The gemstones are localized features in the atmosphere: regions where temperature, composition, or atmospheric height depart from the average. The team found one exactly where theory and previous modeling said it should be, on the evening side of WASP-17b's equator, where powerful wind jets transport heat from the permanently illuminated dayside around toward the shadowed night side, inflating the atmosphere relative to the cooler morning side.
A deformed, wind-scoured sphere
The 650-kelvin divide
Morning vs evening temperatures on WASP-17b's limb, measured with transmission strings on JWST data.
Note: Bar widths are illustrative. The 650-kelvin morning-evening difference is the study's headline figure.
The mapped limb is broadly circular but distinctly asymmetrical, with one side more extended than the other. The atmosphere above the evening limb runs hot, freshly carried over from the dayside, while the atmosphere on the morning limb has chilled during its long journey across the dark hemisphere, returning to the dayside only after traversing the night. The measured temperature difference of about 650 kelvin between the cooler western morning limb and the blistering eastern evening limb landed almost exactly where models said it should.
WASP-17b was already a well-studied world. In 2023, JWST's Mid-Infrared Instrument found quartz crystals, crystalline silica only about 10 nanometers across, forming directly from gas high in its atmosphere, the first time a specific cloud species had been identified on a transiting exoplanet. The new map adds structure to that chemistry: temperatures, composition, and atmospheric height shifting from equator to poles and from day to night, consistent both with theoretical predictions and with other modeling techniques.
Together, the findings assemble one of the most comprehensive three-dimensional views of any exoplanet atmosphere obtained to date. With more than 6,000 exoplanets now confirmed, a verified, spatially resolved case study gives modelers something they have never had: a real atmospheric geometry against which simulations of circulation, radiative transfer, and chemistry can be tested.
Why a shape matters

Part of the significance is technical. JWST's sensitivity has already enabled eclipse mapping, which measures changes in light as an exoplanet swings behind its host star to reveal heat distribution on the dayside. Transmission strings complements that by resolving the limb during transit, capturing the terminator and nightside structure that eclipse mapping cannot reach. Two different vantage points, one coherent picture.
The broader shift is conceptual. For a field that spent decades inferring the properties of alien worlds from averaged, one-dimensional spectra, the ability to see a planet's atmospheric structure directly is a genuine turning point. As Wakeford noted, it is remarkable that the disparate measurements cohered into a structured, dynamical picture of a giant world more than a thousand light-years away, and the method is already beginning to differentiate atmospheric conditions across exoplanet latitudes, moving beyond the simple day-and-night dichotomy.
The research analyzed data from JWST's Deep Reconnaissance of Exoplanet Atmospheres through Multi-instrument Spectroscopy (TST DREAMS) Guaranteed Time Observations program, funded by NASA, the UK Research and Innovation Science and Technology Facilities Council, and the Klarman Fellowship. Its authors describe it as a first step toward resolving weather-scale patterns in exoplanet climates: the winds, storms, and circulation cells that models predict but observations have never directly captured. As the technique is applied to a growing sample of transiting planets, transits become scans of alien weather systems, and the era of the idealized circle is effectively over.
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