Detection of H<sub>2</sub>O and CO<sub>2</sub> in the Atmosphere of the Hot Super-Neptune WASP-166b with JWST

Abstract We characterize the atmosphere of the hot super-Neptune WASP-166b ( P = 5.44 days, R p = 6.9 ± 0.3 R ⊕ , M p = 32.1 ± 1.6 M ⊕ , T eq = 1270 ± 30 K) orbiting an F9V star using JWST transmission spectroscopy with NIRISS and NIRSpec (0.85–5.17 μ m). With this broad wavelength range, NIRISS provides strong constraints on H 2 O and clouds (where NIRSpec performs poorly) while NIRSpec captures CO 2 and NH 3 (where NIRISS performs poorly). Our POSEIDON free chemistry retrievals confirm the detection of H 2 O (15.2 σ significance) and detect CO 2 (14.7 σ ) for the first time. We also find a possible hint of NH 3 (2.3 σ ) and an intermediate pressure cloud deck (2.6 σ ). Finally, we report inconclusive support for the presence of SO 2 , CO, and Na, as well as nondetections of CH 4 , C 2 H 2 , HCN, H 2 S, and K. We verify our results using a TauREx free chemistry retrieval. We also measure with POSEIDON equilibrium chemistry retrievals a superstellar planetary atmospheric metallicity ( <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mi>log</mml:mi> <mml:mo stretchy="false">(</mml:mo> <mml:mi>Z</mml:mi> <mml:mo stretchy="false">)</mml:mo> <mml:mo>=</mml:mo> <mml:mn>1.5</mml:mn> <mml:msubsup> <mml:mrow> <mml:mn>7</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>−</mml:mo> <mml:mn>0.18</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>+</mml:mo> <mml:mn>0.17</mml:mn> </mml:mrow> </mml:msubsup> </mml:math> , <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mi>Z</mml:mi> <mml:mo>=</mml:mo> <mml:mn>3</mml:mn> <mml:msubsup> <mml:mrow> <mml:mn>7</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>−</mml:mo> <mml:mn>13</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>+</mml:mo> <mml:mn>18</mml:mn> </mml:mrow> </mml:msubsup> </mml:math> ) and planetary C/O ratio ( <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mi mathvariant="normal">C</mml:mi> <mml:mo>/</mml:mo> <mml:mi mathvariant="normal">O</mml:mi> <mml:mo>=</mml:mo> <mml:mn>0.28</mml:mn> <mml:msubsup> <mml:mn>2</mml:mn> <mml:mrow> <mml:mo>−</mml:mo> <mml:mn>0.053</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>+</mml:mo> <mml:mn>0.078</mml:mn> </mml:mrow> </mml:msubsup> </mml:math> ) consistent with the stellar C/O ratio (C/O * = 0.41 ± 0.08). These results are compatible with various planetary formation pathways, especially those that include planetesimal accretion followed by core erosion or photoevaporation. WASP-166b also resides near the edge of the Hot Neptune Desert, a sparse population of intermediate-sized planets at high insolation fluxes; thus, these results and further atmospheric observations of Hot Neptunes will help determine the driving processes in the formation of the Hot Neptune Desert.

Authors

Institutions

Publication Details

Journal
The Astronomical Journal
Published
2025-06-24
DOI
https://doi.org/10.3847/1538-3881/adda2e
Citations
7
Primary Topic
Astro and Planetary Science
Type
article
Field-Weighted Citation Impact
8.08

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Detection of H2O and CO2 in the Atmosphere of the Hot Super-Neptune WASP-166b with JWST

Charles D. Fortenbach, Dana R. Louie, Andrew W. Mayo, Steven Giacalone et al.
7 citations
The Astronomical Journal
Astro and Planetary Science
8.08
article

Detection of H2O and CO2 in the Atmosphere of the Hot Super-Neptune WASP-166b with JWST

Charles D. Fortenbach, Dana R. Louie, Andrew W. Mayo, Steven Giacalone, Courtney D. Dressing, Caleb K. Harada, Emma V. Turtelboom
article en
7 citations

Abstract

Abstract We characterize the atmosphere of the hot super-Neptune WASP-166b ( P = 5.44 days, R p = 6.9 ± 0.3 R ⊕ , M p = 32.1 ± 1.6 M ⊕ , T eq = 1270 ± 30 K) orbiting an F9V star using JWST transmission spectroscopy with NIRISS and NIRSpec (0.85–5.17 μ m). With this broad wavelength range, NIRISS provides strong constraints on H 2 O and clouds (where NIRSpec performs poorly) while NIRSpec captures CO 2 and NH 3 (where NIRISS performs poorly). Our POSEIDON free chemistry retrievals confirm the detection of H 2 O (15.2 σ significance) and detect CO 2 (14.7 σ ) for the first time. We also find a possible hint of NH 3 (2.3 σ ) and an intermediate pressure cloud deck (2.6 σ ). Finally, we report inconclusive support for the presence of SO 2 , CO, and Na, as well as nondetections of CH 4 , C 2 H 2 , HCN, H 2 S, and K. We verify our results using a TauREx free chemistry retrieval. We also measure with POSEIDON equilibrium chemistry retrievals a superstellar planetary atmospheric metallicity ( <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mi>log</mml:mi> <mml:mo stretchy="false">(</mml:mo> <mml:mi>Z</mml:mi> <mml:mo stretchy="false">)</mml:mo> <mml:mo>=</mml:mo> <mml:mn>1.5</mml:mn> <mml:msubsup> <mml:mrow> <mml:mn>7</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>−</mml:mo> <mml:mn>0.18</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>+</mml:mo> <mml:mn>0.17</mml:mn> </mml:mrow> </mml:msubsup> </mml:math> , <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mi>Z</mml:mi> <mml:mo>=</mml:mo> <mml:mn>3</mml:mn> <mml:msubsup> <mml:mrow> <mml:mn>7</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>−</mml:mo> <mml:mn>13</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>+</mml:mo> <mml:mn>18</mml:mn> </mml:mrow> </mml:msubsup> </mml:math> ) and planetary C/O ratio ( <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" overflow="scroll"> <mml:mi mathvariant="normal">C</mml:mi> <mml:mo>/</mml:mo> <mml:mi mathvariant="normal">O</mml:mi> <mml:mo>=</mml:mo> <mml:mn>0.28</mml:mn> <mml:msubsup> <mml:mn>2</mml:mn> <mml:mrow> <mml:mo>−</mml:mo> <mml:mn>0.053</mml:mn> </mml:mrow> <mml:mrow> <mml:mo>+</mml:mo> <mml:mn>0.078</mml:mn> </mml:mrow> </mml:msubsup> </mml:math> ) consistent with the stellar C/O ratio (C/O * = 0.41 ± 0.08). These results are compatible with various planetary formation pathways, especially those that include planetesimal accretion followed by core erosion or photoevaporation. WASP-166b also resides near the edge of the Hot Neptune Desert, a sparse population of intermediate-sized planets at high insolation fluxes; thus, these results and further atmospheric observations of Hot Neptunes will help determine the driving processes in the formation of the Hot Neptune Desert.

The Astronomical JournalVol. 170(1)
California Institute of Technology (US), Goddard Space Flight Center (US), University of America (US), San Francisco State University (US), Catholic University of America (US), University of California, Berkeley (US)
Space Telescope Science Institute
Openalex Percentile: Top 3%
Astro and Planetary Science
8.08
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.