Highly irradiated gas giant exoplanets are predicted to show circulation patterns dominated by day-to-night heat transport and a spatial distribution of clouds that is driven by advection and local heating. Hot Jupiters have been extensively studied from broadband phase-curve observations at infrared and optical wavelengths, but spectroscopic observations in the reflected light are rare and the regime of smaller and higher-metallicity ultrahot planets, such as hot Neptunes, remains largely unexplored. Here we present the phase-resolved reflected light and thermal emission spectroscopy of the ultrahot Neptune LTT 9779 b, obtained through observing its full phase curve from 0.6 μm to 2.8 μm with the NIRISS/SOSS instrument onboard the JWST. We detect an asymmetric dayside in reflected light (3.1σ significance) with highly reflective white clouds on the western dayside (albedo A = 0.79 ± 0.15) and a much lower-albedo eastern dayside (A = 0.41 ± 0.10), resulting in an overall dayside albedo of A = 0.50 ± 0.07. The thermal phase curve is symmetric about the substellar point, with a dayside effective temperature of <InlineEquation ID="IEq1"> <InlineMediaObject> <ImageObject Color="BlackWhite" FileRef="41550_2025_2488_Article_IEq1.gif" Format="GIF" Height="22" Rendition="HTML" Resolution="72" Type="Linedraw" Width="144" /> </InlineMediaObject> <EquationSource Format="TEX">${{{T}}}_{{\rm{eff}},{\rm{day}}}={\mathrm{2,260}}_{-50}^{+40}\,{\mathrm{K}}$</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <msub> <mrow> <mi>T</mi> </mrow> <mrow> <mi mathvariant="normal">eff</mi> <mo>,</mo> <mi mathvariant="normal">day</mi> </mrow> </msub> <mo>=</mo> <msubsup> <mrow> <mi mathvariant="normal">2,260</mi> </mrow> <mrow> <mo>−</mo> <mn>50</mn> </mrow> <mrow> <mo>+</mo> <mn>40</mn> </mrow> </msubsup> <mspace width="0.25em" /> <mi mathvariant="normal">K</mi> </mrow> </math></EquationSource> </InlineEquation> and a cold nightside (Teff,night < 1,330 K at 3σ confidence), indicative of short radiative timescales. We propose an atmospheric circulation and cloud distribution regime in which heat is transported eastwards from the dayside towards the cold nightside by an equatorial jet, leading to a colder western dayside where temperatures are sufficiently low for the condensation of silicate clouds.

Highly reflective white clouds on the western dayside of an exo-Neptune

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发表日期：

2025年2月25日

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Louis-Philippe Coulombe,
Michael Radica,
Björn Benneke,
Élyse D’Aoust,
Lisa Dang,
Nicolas B. Cowan,
Vivien Parmentier,
Loïc Albert,
David Lafrenière,
Jake Taylor,
Pierre-Alexis Roy,
Stefan Pelletier,
Romain Allart,
Étienne Artigau,
René Doyon,
Ray Jayawardhana,
Doug Johnstone,
Lisa Kaltenegger,
Adam B. Langeveld,
Ryan J. MacDonald,
Jason F. Rowe,
Jake D. Turner

摘要

Highly irradiated gas giant exoplanets are predicted to show circulation patterns dominated by day-to-night heat transport and a spatial distribution of clouds that is driven by advection and local heating. Hot Jupiters have been extensively studied from broadband phase-curve observations at infrared and optical wavelengths, but spectroscopic observations in the reflected light are rare and the regime of smaller and higher-metallicity ultrahot planets, such as hot Neptunes, remains largely unexplored. Here we present the phase-resolved reflected light and thermal emission spectroscopy of the ultrahot Neptune LTT 9779 b, obtained through observing its full phase curve from 0.6 μm to 2.8 μm with the NIRISS/SOSS instrument onboard the JWST. We detect an asymmetric dayside in reflected light (3.1σ significance) with highly reflective white clouds on the western dayside (albedo A = 0.79 ± 0.15) and a much lower-albedo eastern dayside (A = 0.41 ± 0.10), resulting in an overall dayside albedo of A = 0.50 ± 0.07. The thermal phase curve is symmetric about the substellar point, with a dayside effective temperature of ${{{T}}}_{{\rm{eff}},{\rm{day}}}={\mathrm{2,260}}_{-50}^{+40}\,{\mathrm{K}}$ $T_{eff, day} = {2,260}_{- 50}^{+ 40} K$ and a cold nightside (T_eff,night < 1,330 K at 3σ confidence), indicative of short radiative timescales. We propose an atmospheric circulation and cloud distribution regime in which heat is transported eastwards from the dayside towards the cold nightside by an equatorial jet, leading to a colder western dayside where temperatures are sufficiently low for the condensation of silicate clouds.