Atmospheric asymmetries in WASP-121 b revealed by rotational transits detected with JWST
Pith reviewed 2026-06-26 19:04 UTC · model grok-4.3
The pith
Two transits of WASP-121 b show asymmetric light curves from the planet's rotation, with rising CO absorption indicating higher eastern dayside temperatures.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
The central claim is that the two observed transits exhibit asymmetric light curves caused by WASP-121 b's rotation, with the transmission spectrum showing increasing CO absorption and slightly decreasing H2O absorption as the planet rotates; these changes indicate a stronger longitudinal temperature gradient across the evening terminator than the morning terminator, consistent with higher temperatures in the eastern half than the western half of the dayside.
What carries the argument
Rotational transit, the effect in which the planet's spin during the transit progressively exposes different longitudinal slices of its atmosphere to the line of sight.
If this is right
- The evening terminator exhibits a stronger longitudinal temperature gradient than the morning terminator.
- Higher eastern dayside temperatures drive thermal dissociation of H2O while leaving CO largely intact.
- Longitudinal gradients of temperature and chemistry can be constrained from rotational phase coverage during a single transit.
- This provides a probe of atmospheric heterogeneity that is distinct from limb-asymmetry measurements between morning and evening terminators.
Where Pith is reading between the lines
- Similar rotational signatures may be detectable in other ultra-hot Jupiters observed with JWST at high cadence.
- Ignoring rotational effects could bias retrievals of average terminator properties when phase coverage is good.
- Multi-transit campaigns could map the full dayside temperature distribution by stacking rotational signals.
Load-bearing premise
The observed changes in transmission spectrum with orbital phase are produced by the planet's rotation bringing different atmospheric regions into view rather than by instrumental systematics or orbital dynamics.
What would settle it
A third transit or re-reduction of the existing data that shows no phase-dependent change in CO or H2O absorption depths, or that reproduces the asymmetry with a model containing only instrumental or limb-darkening effects.
read the original abstract
Close-in exoplanets are tidally locked to their host star and thus exhibit extreme atmospheric temperature gradients. It has been theorized that the fraction of star light absorbed by such planets during transit changes as a function of orbital phase as progressively hotter or colder atmospheric gas rotates into view, but this effect has not been observed so far. Here, we show that two transits of the ultra-hot Jupiter WASP-121 b, acquired with JWST/NIRSpec and NIRISS, exhibit asymmetric transit light curves caused by the planet's rotation during transit. We observe increasing CO absorption and slightly decreasing H$_2$O absorption in the transmission spectrum, as the planet rotates. These results are indicative of a stronger longitudinal temperature gradient across the evening than across the morning terminator, consistent with higher temperatures in the eastern half than in the western half of the dayside. The observed changes of the transmission spectrum with orbital phase are in line with the temperature increase causing thermal dissociation of H$_2$O, while CO remains abundant. The observation of longitudinal gradients of atmospheric temperature and chemistry from the planet's rotational transit provides a new probe for constraining atmospheric heterogeneity using JWST beyond differences between morning and evening terminators from limb asymmetries.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The paper claims detection of asymmetric transit light curves in two JWST/NIRSpec and NIRISS observations of WASP-121 b, attributed to the planet's rotation during transit bringing different longitudes into view. It reports increasing CO absorption and slightly decreasing H2O absorption with orbital phase, interpreted as evidence for a stronger longitudinal temperature gradient across the evening terminator than the morning one, consistent with higher eastern dayside temperatures and thermal dissociation of H2O while CO remains stable. This is presented as a new probe of atmospheric heterogeneity beyond standard limb asymmetries.
Significance. If the attribution of the asymmetries and spectral changes specifically to rotational effects holds after rigorous testing, the result would be significant for the field: it demonstrates a novel JWST-accessible method to constrain east-west atmospheric gradients and chemistry in tidally locked ultra-hot Jupiters, providing empirical tests of 3D circulation and dissociation models that were previously only theoretical.
major comments (2)
- [Abstract and §3] Abstract and §3 (light-curve analysis): the central claim that the observed transit asymmetries are caused by planetary rotation (rather than residual JWST systematics, limb-darkening inaccuracies, or orbital geometry effects) is load-bearing but lacks quantitative demonstration that the asymmetry amplitude matches the expected rotational contribution given the known spin period and scale height; without this, the causal link remains at risk.
- [§4] §4 (transmission spectra): the interpretation of phase-dependent CO increase / H2O decrease as indicating a stronger evening-terminator gradient requires forward-modeling comparisons showing that the observed spectral changes exceed those expected from unmodeled limb asymmetries or chemistry variations unrelated to the claimed east-west dayside gradient; the current evidence appears post-hoc.
minor comments (3)
- Clarify the exact orbital phases of the two transits and the binning choices for the phase-resolved spectra to allow reproducibility.
- Add explicit references to prior theoretical work on rotational transit effects in ultra-hot Jupiters for context.
- Ensure error bars on the reported absorption changes account for correlated noise in the JWST time series.
Simulated Author's Rebuttal
We thank the referee for their constructive comments. We address each major comment below and indicate planned revisions to strengthen the manuscript.
read point-by-point responses
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Referee: [Abstract and §3] Abstract and §3 (light-curve analysis): the central claim that the observed transit asymmetries are caused by planetary rotation (rather than residual JWST systematics, limb-darkening inaccuracies, or orbital geometry effects) is load-bearing but lacks quantitative demonstration that the asymmetry amplitude matches the expected rotational contribution given the known spin period and scale height; without this, the causal link remains at risk.
Authors: We agree that a quantitative demonstration is important to solidify the attribution to rotation. In the revised manuscript we will add to §3 an explicit calculation of the expected asymmetry amplitude using the known spin period, transit duration, and scale height of WASP-121 b. This will show that the observed asymmetry is consistent in magnitude with the rotational contribution, helping to distinguish it from systematics or geometric effects. revision: yes
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Referee: [§4] §4 (transmission spectra): the interpretation of phase-dependent CO increase / H2O decrease as indicating a stronger evening-terminator gradient requires forward-modeling comparisons showing that the observed spectral changes exceed those expected from unmodeled limb asymmetries or chemistry variations unrelated to the claimed east-west dayside gradient; the current evidence appears post-hoc.
Authors: We acknowledge the value of forward-modeling comparisons. While a full 3D forward model lies beyond the present scope, the revised §4 will include a semi-quantitative estimate showing that the observed CO increase and H2O decrease exceed the amplitude expected from limb asymmetries alone and align with the expected effects of a stronger evening-terminator temperature gradient and H2O dissociation. This addition will make the interpretation less post-hoc. revision: partial
Circularity Check
No significant circularity; claims are observational interpretations of JWST data
full rationale
The paper reports direct JWST observations of asymmetric transit light curves and phase-dependent spectral changes in WASP-121 b, attributing them to rotational effects via comparison with expected atmospheric gradients. No derivation chain, equations, or predictions reduce to inputs by construction; there are no self-definitional parameters, fitted inputs renamed as predictions, or load-bearing self-citations that force the result. The interpretation rests on external physical expectations rather than internal redefinition, qualifying as self-contained empirical analysis.
Axiom & Free-Parameter Ledger
axioms (2)
- domain assumption Close-in exoplanets are tidally locked and exhibit extreme atmospheric temperature gradients.
- domain assumption Temperature increase causes thermal dissociation of H2O while CO remains abundant.
Reference graph
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