📄 JWST/NIRISS Reveals the Water-rich "Steam World" Atmosphere of GJ 982…

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Piaulet-Ghorayeb, Caroline et al. (2024) · The Astrophysical Journal
Reads: 417 · Citations: 91
DOI: 10.3847/2041-8213/ad6f00

🔗 https://ui.adsabs.harvard.edu/abs/2024ApJ...974L..10P/abstract

#Astronomy #Astrophysics #Galaxies #SolarPhysics #ExoplanetAtmospheres

JWST/NIRISS Reveals the Water-rich "Steam World" Atmosphere of GJ 9827 d

With sizable volatile envelopes but smaller radii than the solar system ice giants, sub-Neptunes have been revealed as one of the most common types of planet in the galaxy. While the spectroscopic characterization of larger sub-Neptunes (2.5─4 R <SUB>⊕</SUB>) has revealed hydrogen-dominated atmospheres, smaller sub-Neptunes (1.6─2.5 R <SUB>⊕</SUB>) could either host thin, rapidly evaporating, hydrogen-rich atmospheres or be stable, metal-rich "water worlds" with high mean molecular weight atmospheres and a fundamentally different formation and evolutionary history. Here, we present the 0.6─2.8 μm JWST/NIRISS/SOSS transmission spectrum of GJ 9827 d, the smallest (1.98 R <SUB>⊕</SUB>) warm (T <SUB>eq,A=0.3</SUB> ∼ 620 K) sub-Neptune where atmospheric absorbers have been detected to date. Our two transit observations with NIRISS/SOSS, combined with the existing HST/WFC3 spectrum, enable us to break the clouds─metallicity degeneracy. We detect water in a highly metal-enriched "steam world" atmosphere (O/H of ∼4 by mass and H<SUB>2</SUB>O found to be the background gas with a volume mixing ratio of >31%). We further show that these results are robust to stellar contamination through the transit light source effect. We do not detect escaping metastable He, which, combined with previous nondetections of escaping He and H, supports the steam atmosphere scenario. In water-rich atmospheres, hydrogen loss driven by water photolysis happens predominantly in the ionized form, which eludes observational constraints. We also detect several flares in the NIRISS/SOSS light curves with far-UV energies of the order of 10<SUP>30</SUP> erg, highlighting the active nature of the star. Further atmospheric characterization of GJ 9827 d probing carbon or sulfur species could reveal the origin of its high metal enrichment.

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A Final Look at The Roman Space Telescope's Primary Mirror: Beauty Shots 🌑🛰️🧑‍🚀

#Africa #Artemis #Astronaut #Cleanroom #EarthScience #Exoplanet #ExoplanetAtmospheres #Hardware

⏩ 5 new pictures and 8 new videos from NASA (SVS) https://commons.wikimedia.org/wiki/Special:ListFiles?limit=31&user=OptimusPrimeBot&ilshowall=1&offset=20260423175839

📄 Carbon-bearing Molecules in a Possible Hycean Atmosphere

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Madhusudhan, Nikku et al. (2023) · The Astrophysical Journal
Reads: 549 · Citations: 235
DOI: 10.3847/2041-8213/acf577

🔗 https://ui.adsabs.harvard.edu/abs/2023ApJ...956L..13M/abstract

#Astronomy #Astrophysics #Exoplanets #HabitablePlanets #ExoplanetAtmospheres

Carbon-bearing Molecules in a Possible Hycean Atmosphere

The search for habitable environments and biomarkers in exoplanetary atmospheres is the holy grail of exoplanet science. The detection of atmospheric signatures of habitable Earth-like exoplanets is challenging owing to their small planet–star size contrast and thin atmospheres with high mean molecular weight. Recently, a new class of habitable exoplanets, called Hycean worlds, has been proposed, defined as temperate ocean-covered worlds with H<SUB>2</SUB>-rich atmospheres. Their large sizes and extended atmospheres, compared to rocky planets of the same mass, make Hycean worlds significantly more accessible to atmospheric spectroscopy with JWST. Here we report a transmission spectrum of the candidate Hycean world K2-18 b, observed with the JWST NIRISS and NIRSpec instruments in the 0.9–5.2 μm range. The spectrum reveals strong detections of methane (CH<SUB>4</SUB>) and carbon dioxide (CO<SUB>2</SUB>) at 5σ and 3σ confidence, respectively, with high volume mixing ratios of ∼1% each in a H<SUB>2</SUB>-rich atmosphere. The abundant CH<SUB>4</SUB> and CO<SUB>2</SUB>, along with the nondetection of ammonia (NH<SUB>3</SUB>), are consistent with chemical predictions for an ocean under a temperate H<SUB>2</SUB>-rich atmosphere on K2-18 b. The spectrum also suggests potential signs of dimethyl sulfide (DMS), which has been predicted to be an observable biomarker in Hycean worlds, motivating considerations of possible biological activity on the planet. The detection of CH<SUB>4</SUB> resolves the long-standing missing methane problem for temperate exoplanets and the degeneracy in the atmospheric composition of K2-18 b from previous observations. We discuss possible implications of the findings, open questions, and future observations to explore this new regime in the search for life elsewhere.

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