A JWST NIRSpec Phase Curve for WASP-121b: Dayside Emission Strongest Eastward of the Substellar Point and Nightside Conditions Conducive to Cloud …

T Mikal-Evans, DK Sing, J Dong… - The Astrophysical …, 2023 - iopscience.iop.org
T Mikal-Evans, DK Sing, J Dong, D Foreman-Mackey, T Kataria, JK Barstow, JM Goyal
The Astrophysical Journal Letters, 2023iopscience.iop.org
We present the first exoplanet phase-curve measurement made with the JWST NIRSpec
instrument, highlighting the exceptional stability of this newly commissioned observatory for
exoplanet climate studies. The target, WASP-121b, is an ultrahot Jupiter with an orbital
period of 30.6 hr. We analyze two broadband light curves generated for the NRS1 and
NRS2 detectors, covering wavelength ranges of 2.70–3.72 μm and 3.82–5.15 μm,
respectively. Both light curves exhibit minimal systematics, with approximately linear drifts in …
Abstract
We present the first exoplanet phase-curve measurement made with the JWST NIRSpec instrument, highlighting the exceptional stability of this newly commissioned observatory for exoplanet climate studies. The target, WASP-121b, is an ultrahot Jupiter with an orbital period of 30.6 hr. We analyze two broadband light curves generated for the NRS1 and NRS2 detectors, covering wavelength ranges of 2.70–3.72 μm and 3.82–5.15 μm, respectively. Both light curves exhibit minimal systematics, with approximately linear drifts in the baseline flux level of 30 ppm hr− 1 (NRS1) and 10 ppm hr− 1 (NRS2). Assuming a simple brightness map for the planet described by a low-order spherical harmonic dipole, our light-curve fits suggest that the phase curve peaks coincide with orbital phases 3 fdg 36±0 fdg 11 (NRS1) and 2 fdg 66±0 fdg 12 (NRS2) prior to mideclipse. This is consistent with the strongest dayside emission emanating from eastward of the substellar point. We measure planet-to-star emission ratios of 3924±7 ppm (NRS1) and 4924±9 ppm (NRS2) for the dayside hemisphere and 136±8 ppm (NRS1) and 630±10 ppm (NRS2) for the nightside hemisphere. The latter nightside emission ratios translate to planetary brightness temperatures of 926±12 K (NRS1) and 1122±10 K (NRS2), which are low enough for a wide range of refractory condensates to form, including enstatite and forsterite. A nightside cloud deck may be blocking emission from deeper, hotter layers of the atmosphere, potentially helping to explain why cloud-free 3D general circulation model simulations systematically overpredict the nightside emission for WASP-121b.
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