Transmission spectroscopy is the primary technique used by jwst and its precursors to characterize exoplanet atmospheres. During a planetary transit, starlight passes through the thin limb of the planet’s atmosphere; absorption features imprinted on the stellar spectrum reveal atmospheric composition at specific pressure levels along the terminator.

Transmission spectra are 1D averages of intrinsically 3D atmospheric structure — a fundamental methodological limit emphasized by sara-seager et al. (src-jwst-biosignature-prospects-2025). The 1D-versus-3D mismatch contributes to the “parallel interpretations” problem in biosignature retrieval, in which the same spectrum admits multiple consistent atmospheric models. JWST can access only a handful of habitable-zone atmospheres before hitting its noise floor.

The limb-resolved jwst study of hot-jupiter wasp-94ab (Mukherjee & Sing, Science, May 2026) is the most concrete demonstration of this limit: the planet’s leading (morning) and trailing (evening) limbs enter and exit transit at different times, so their spectra can be measured separately. Doing so revealed a cloudy morning limb and a clear evening limb — and corrected the planet’s inferred oxygen/carbon abundance from “hundreds of times” Jupiter (blended) to ~5× Jupiter (limb-resolved), a >4σ shift (src-jwst-wasp-94ab-weather-cycle-2026-05).

Beyond biosignature retrieval, transmission-spectrum metallicity, C/O ratio, and mean molecular weight constrain planetary formation pathway. The jwst toi-1130b retrieval (Barat et al., 2026) is a methodological reference: a high-mean-molecular-weight-atmosphere (μ = 5.5 amu) plus high metallicity supports ex-situ formation beyond the water-ice-line for that warm mini-neptune (src-jwst-toi-1130b-atmosphere-2026-05).

A related rotational-transit (limb-resolved) variant converts elapsed transit time into longitude on the rotating planet, mapping how the spectrum changes across the terminator. The jwst study of wasp-121b (Gapp et al., Nature Astronomy 2026) used it to probe ~30° of rotation and resolve a dawn–dusk atmospheric asymmetry (src-jwst-wasp-121b-dawn-dusk-2026-06).

Contrasts with direct-imaging, where the planet is resolved from its host star and its emitted or reflected spectrum is measured directly (target of habitable-worlds-observatory and LIFE).

Lunine & Bahcall survey validation (PNAS, 2025)

A PNAS overview by Lunine (JPL/Caltech) and Bahcall (Princeton) (src-pnas-jwst-exoplanet-characterization-era-2025) identifies transmission spectroscopy — both primary transit and secondary eclipse (emission) variants — as the enabling method behind JWST’s infrared sensitivity advantage over all prior facilities. The survey documents JWST achieving transmission spectra of planets with radii nearly as small as Earth’s, unprecedented in the field. It also notes that despite characterizing 10 rocky Earth-sized planets, JWST has made no definitive atmospheric detection on any of them — transmission spectroscopy is a necessary but not sufficient tool for rocky-planet characterization.