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Transiting exoplanets orbiting young nearby stars are ideal laboratories for testing theories of planet formation and evolution. However, to date only a handful of stars with age, submitted to MNRAS

The abundance of refractory elements in giant planets can provide key insights into their formation histories. Due to the Solar System giants' low temperatures, refractory elements condense below the cloud deck limiting sensing capabilities to only highly volatile elements. Recently, ultra-hot giant exoplanets have allowed for some refractory elements to be measured showing abundances broadly consistent with the solar nebula with titanium likely condensed out of the photosphere. Here we report precise abundance constraints of 14 major refractory elements on the ultra-hot giant planet WASP-76b that show distinct deviations from proto-solar, and a sharp onset in condensation temperature. In particular, we find nickel to be enriched, a possible sign of the accretion of a differentiated object's core during the planet's evolution. Elements with condensation temperatures below 1,550 K otherwise closely match those of the Sun before sharply transitioning to being strongly depleted above 1,550 K, well explained by nightside cold-trapping. We further unambiguously detect vanadium oxide on WASP-76b, a molecule long hypothesized to drive atmospheric thermal inversions, and also observe a global east-west asymmetry in its absorption signals. Overall, our findings indicate that giant planets have a mostly stellar-like refractory elemental content and suggest that temperature sequences of hot Jupiter spectra can show abrupt transitions wherein a mineral species is either present, or completely absent if a cold-trap exists below its condensation temperature., Published online in Nature on June 14, 2023

Close-in giant exoplanets with temperatures greater than 2,000 K (''ultra-hot Jupiters'') have been the subject of extensive efforts to determine their atmospheric properties using thermal emission measurements from the Hubble and Spitzer Space Telescopes. However, previous studies have yielded inconsistent results because the small sizes of the spectral features and the limited information content of the data resulted in high sensitivity to the varying assumptions made in the treatment of instrument systematics and the atmospheric retrieval analysis. Here we present a dayside thermal emission spectrum of the ultra-hot Jupiter WASP-18b obtained with the NIRISS instrument on JWST. The data span 0.85 to 2.85 $\mu$m in wavelength at an average resolving power of 400 and exhibit minimal systematics. The spectrum shows three water emission features (at $>$6$\sigma$ confidence) and evidence for optical opacity, possibly due to H$^-$, TiO, and VO (combined significance of 3.8$\sigma$). Models that fit the data require a thermal inversion, molecular dissociation as predicted by chemical equilibrium, a solar heavy element abundance (''metallicity'', M/H = 1.03$_{-0.51}^{+1.11}$ $\times$ solar), and a carbon-to-oxygen (C/O) ratio less than unity. The data also yield a dayside brightness temperature map, which shows a peak in temperature near the sub-stellar point that decreases steeply and symmetrically with longitude toward the terminators., Comment: JWST ERS bright star observations. Uploaded to inform JWST Cycle 2 proposals. Manuscript under review. 50 pages, 14 figures, 2 tables

Photochemistry is a fundamental process of planetary atmospheres that regulates the atmospheric composition and stability. However, no unambiguous photochemical products have been detected in exoplanet atmospheres to date. Recent observations from the JWST Transiting Exoplanet Early Release Science Program found a spectral absorption feature at 4.05 $\mu$m arising from SO$_2$ in the atmosphere of WASP-39b. WASP-39b is a 1.27-Jupiter-radii, Saturn-mass (0.28 M$_J$) gas giant exoplanet orbiting a Sun-like star with an equilibrium temperature of $\sim$1100 K. The most plausible way of generating SO$_2$ in such an atmosphere is through photochemical processes. Here we show that the SO$_2$ distribution computed by a suite of photochemical models robustly explains the 4.05 $\mu$m spectral feature identified by JWST transmission observations with NIRSpec PRISM (2.7$\sigma$) and G395H (4.5$\sigma$). SO$_2$ is produced by successive oxidation of sulphur radicals freed when hydrogen sulphide (H$_2$S) is destroyed. The sensitivity of the SO$_2$ feature to the enrichment of the atmosphere by heavy elements (metallicity) suggests that it can be used as a tracer of atmospheric properties, with WASP-39b exhibiting an inferred metallicity of $\sim$10$\times$ solar. We further point out that SO$_2$ also shows observable features at ultraviolet and thermal infrared wavelengths not available from the existing observations., Comment: 39 pages, 14 figures, accepted to be published in Nature

Carbon dioxide (CO2) is a key chemical species that is found in a wide range of planetary atmospheres. In the context of exoplanets, CO2 is an indicator of the metal enrichment (i.e., elements heavier than helium, also called "metallicity"), and thus formation processes of the primary atmospheres of hot gas giants. It is also one of the most promising species to detect in the secondary atmospheres of terrestrial exoplanets. Previous photometric measurements of transiting planets with the Spitzer Space Telescope have given hints of the presence of CO2 but have not yielded definitive detections due to the lack of unambiguous spectroscopic identification. Here we present the detection of CO2 in the atmosphere of the gas giant exoplanet WASP-39b from transmission spectroscopy observations obtained with JWST as part of the Early Release Science Program (ERS). The data used in this study span 3.0 to 5.5 {\mu}m in wavelength and show a prominent CO2 absorption feature at 4.3 {\mu}m (26{\sigma} significance). The overall spectrum is well matched by one-dimensional, 10x solar metallicity models that assume radiative-convective-thermochemical equilibrium and have moderate cloud opacity. These models predict that the atmosphere should have water, carbon monoxide, and hydrogen sulfide in addition to CO2, but little methane. Furthermore, we also tentatively detect a small absorption feature near 4.0 {\mu}m that is not reproduced by these models., Comment: 27 pages, 6 figures, Accepted for publication in Nature, data and models available at https://doi.10.5281/zenodo.6959427

Photochemistry is a fundamental process of planetary atmospheres that is integral to habitability, atmospheric composition and stability, and aerosol formation. However, no unambiguous photochemical products have been detected in exoplanet atmospheres to date. Here we show that photochemically produced sulphur dioxide (SO2) is present in the atmosphere of the hot, giant exoplanet WASP-39b, as constrained by data from the JWST Transiting Exoplanet Early Release Science Program and informed by a suite of photochemical models. We find that SO2 is produced by successive oxidation of sulphur radicals freed when hydrogen sulphide (H2S) is destroyed. The SO2 distribution computed by the photochemical models robustly explains the 4.05 μm spectral feature seen in JWST transmission spectra [Rustamkulov et al.(submitted), Alderson et al.(submitted)] and leads to observable features at ultraviolet and thermal infrared wavelengths not available from the current observations. The sensitivity of the SO2 feature to the enrichment of heavy elements in the atmosphere ("metallicity") suggests that it can be used as a powerful tracer of atmospheric properties, with our results implying a metallicity of ∼10× solar for WASP-39b. Through providing improved constraints on bulk metallicity and sulphur abundance, the detection of SO2 opens a new avenue for the investigation of giant-planet formation. Our work demonstrates that sulphur photochemistry may be readily observable for exoplanets with super-solar metallicity and equilibrium temperatures ≳750 K. The confirmation of photochemistry through the agreement between theoretical predictions and observational data is pivotal for further atmospheric characterisation studies.

We present a uniform analysis of transit observations from the Hubble Space Telescope and Spitzer Space Telescope of two warm gas giants orbiting K-type stars - WASP-29b and WASP-80b. The transmission spectra, which span 0.4-5.0 $\mu$m, are interpreted using a suite of chemical equilibrium PLATON atmospheric retrievals. Both planets show evidence of significant aerosol opacity along the day-night terminator. The spectrum of WASP-29b is flat throughout the visible and near-infrared, suggesting the presence of condensate clouds extending to low pressures. The lack of spectral features hinders our ability to constrain the atmospheric metallicity and C/O ratio. In contrast, WASP-80b shows a discernible, albeit muted H$_2$O absorption feature at 1.4 $\mu$m, as well as a steep optical spectral slope that is caused by fine-particle aerosols and/or contamination from unocculted spots on the variable host star. WASP-80b joins the small number of gas-giant exoplanets that show evidence for enhanced atmospheric metallicity: the transmission spectrum is consistent with metallicities ranging from $\sim$30-100 times solar in the case of cloudy limbs to a few hundred times solar in the cloud-free scenario. In addition to the detection of water, we infer the presence of CO$_2$ in the atmosphere of WASP-80b based on the enhanced transit depth in the Spitzer 4.5 $\mu$m bandpass. From a complementary analysis of Spitzer secondary eclipses, we find that the dayside emission from WASP-29b and WASP-80b is consistent with brightness temperatures of $937 \pm 48$ and $851 \pm 14$ K, respectively, indicating relatively weak day-night heat transport and low Bond albedo., Comment: Published in AJ, 26 pages, 13 figures. Updated to reflect proof changes

The population of planets smaller than approximately $1.7~R_\oplus$ is widely interpreted as consisting of rocky worlds, generally referred to as super-Earths. This picture is largely corroborated by radial-velocity (RV) mass measurements for close-in super-Earths but lacks constraints at lower insolations. Here we present the results of a detailed study of the Kepler-138 system using 13 Hubble and Spitzer transit observations of the warm-temperate $1.51\pm0.04~R_\oplus$ planet Kepler-138 d ($T_{\mathrm{eq, A_B=0.3}}$~350 K) combined with new Keck/HIRES RV measurements of its host star. We find evidence for a volatile-rich "water world" nature of Kepler-138 d, with a large fraction of its mass contained in a thick volatile layer. This finding is independently supported by transit timing variations, RV observations ($M_d=2.1_{-0.7}^{+0.6}~M_\oplus$), as well as the flat optical/IR transmission spectrum. Quantitatively, we infer a composition of $11_{-4}^{+3}$\% volatiles by mass or ~51% by volume, with a 2000 km deep water mantle and atmosphere on top of a core with an Earth-like silicates/iron ratio. Any hypothetical hydrogen layer consistent with the observations ($, Published in Nature Astronomy. 4 main figures, 10 extended data figures, 13 supplementary figures. 4 tables

The continuous, long-baseline photometry provided by TESS has enabled detailed phase curve studies of planetary systems. Over the course of the two-year Primary Mission, we carried out a systematic light curve analysis of both known targets and newly discovered systems. By measuring the phase curve, we probed fundamental physical quantities, such as the planet’s dayside temperature, Bond albedo, and day-night heat recirculation efficiency, as well as the host star’s response to the mutual star-planet gravitational interaction. In this talk, I provide an overview of the main results from the Primary Mission. We detected phase curves for over 20 targets and combined TESS-band eclipse measurements with Spitzer secondary eclipse depths to obtain self-consistent dayside brightness temperatures and optical geometric albedos. These albedo measurements have revealed an intriguing apparent trend between increasing dayside temperature and increasing geometric albedo for hot Jupiters. With TESS now well into its Extended Mission, we consider possible avenues for follow-up intensive atmospheric characterization and discuss fruitful opportunities for future study as the telescope revisits these systems in the coming years., {"references":["Addison, B.C., Knudstrup, E., Wong, I., et al. 2021, AJ, in revision","Ahlers, J.P., Johnson, M.C., Stassun, K.G., et al. 2020, AJ, 160, 4","Cabot, S.H.C., Bello-Arufe, A., Mendonça, J.M., et al. 2021, AJ, in revision","Mansfield, M., Bean, J.L., Stevenson, K.B., et al. 2020, ApjL, 888, L15","Shporer, A. 2017, PASP, 129, 072001","Shporer, A., Wong, I., Huang, C.X., et al. 2019, AJ, 157, 178","Wong, I., Kitzmann, D., Shporer, A., et al. 2021a, AJ, in press","Wong, I., Shporer, A., Daylan, T. et al. 2020a, AJ, 160, 155","Wong, I., Shporer, A., Kitzmann, D., et al. 2020b, AJ, 160, 88","Wong, I., Shporer, A., Zhou, G., et al. 2021b, AJ, submitted","Zhou, G., Huang, C.X., Bakos, G.Á., et al. 2019, AJ, 158, 141"]}

We validate the presence of a two-planet system orbiting the 0.15--1.4 Gyr K4 dwarf TOI 560 (HD 73583). The system consists of an inner moderately eccentric transiting mini-Neptune (TOI 560 b, $P = 6.3980661^{+0.0000095}_{-0.0000097}$ days, $e=0.294^{+0.13}_{-0.062}$, $M= 0.94^{+0.31}_{-0.23}M_{Nep}$) initially discovered in the Sector 8 \tess\ mission observations, and a transiting mini-Neptune (TOI 560 c, $P = 18.8805^{+0.0024}_{-0.0011}$ days, $M= 1.32^{+0.29}_{-0.32}M_{Nep}$) discovered in the Sector 34 observations, in a rare near-1:3 orbital resonance. We utilize photometric data from \tess\, \textit{Spitzer}, and ground-based follow-up observations to confirm the ephemerides and period of the transiting planets, vet false positive scenarios, and detect the photo-eccentric effect for TOI 560 b. We obtain follow-up spectroscopy and corresponding precise radial velocities (RVs) with the iSHELL spectrograph at the NASA Infrared Telescope Facility and the HIRES Spectrograph at Keck Observatory to validate the planetary nature of these signals, which we combine with published PFS RVs from Magellan Observatory. We detect the masses of both planets at $> 3-σ$ significance. We apply a Gaussian process (GP) model to the \tess\ light curves to place priors on a chromatic radial velocity GP model to constrain the stellar activity of the TOI 560 host star, and confirm a strong wavelength dependence for the stellar activity demonstrating the ability of NIR RVs in mitigating stellar activity for young K dwarfs. TOI 560 is a nearby moderately young multi-planet system with two planets suitable for atmospheric characterization with James Webb Space Telescope (JWST) and other upcoming missions. In particular, it will undergo six transit pairs separated by $, AAS Journals, Accepted for publication

Micro- and nano-satellites offer cost-effective platforms for space technology development and for targeted investigations in astronomy.The original 1999 CubeSat design, based on 1 litre-sized cubes, is now the standard '1U' prototyping architecture.The Canadian Space Agency was an early adopter of micro-satellites.The MOST (Microvariability and Oscillation of Stars) telescope was Canada's first astronomy satellite.Launched in 2003, MOST offered a dedicated platform for asteroseismology that demonstrated the advantages of uninterrupted, long-duration staring observations well before the Kepler Mission adopted the same technique to discover thousands of extrasolar planets.MOST opened the astronomy time domain from space.The subsequent BRITE (BRIght Target Explorer) Constellation was the first space astronomy mission to be carried out with nano-satellites, with Canada designing all and contributing two of the six 8U-sized satellites.Its greatest advantage was its ability to stay pointed on a wide field (24 x 24 degres) monitoring up to 30 bright stellar targets for up to 6 months. Micro-satellite adoption remains slow in astronomy, mostly because of the need for large telescope apertures.However, as demonstrated by MOST and BRITE, time-domain photometry of bright objects, such as Milky Way stars and planetary systems, can be well-served by modest apertures.Improving detector technology is now opening micro-satellite platforms to fainter objects, multi-band photometry, non-optical wavelengths, and polarimetry. Canada is in a strong position to lead micro-satellite astronomy. Building small and cost-effective - but capable - space platforms will ensure that Canada stays at the forefront of space technology development. Focusing on a few key micro-satellite investigations will optimize the science impact of Canadian space astronomy.Early experience with Canadian micro-satellites also enhances Canadian expertise and HQP training for participation in larger international follow-on missions. The Canadian Space Agency currently operates two astronomy small-satellite missions, the Near Earth Object Surveillance Satellite (NEOSSat) and BRIght Target Explorer (BRITE) Constellation, and has two more missions under study: the Photometric Observations of Extrasolar Planets (POEP) and the Extrasolar Planet Polarimetry Explorer / Explorateur Polarimétrique des Planètes Extrasolaires (ÉPPÉ).NEOSSat's first Guest Observer call for proposals in September 2019 was heavily (4.8:1) over-subscribed, reflecting intense astronomy interest. BRITE Constellation has already demonstrated to be one of Canada's highest-publication impact observatories. Both POEP and ÉPPÉ promise novel, science-enabling capabilities in space-based time-domain astronomy with applications well beyond their primary exoplanet-focused goals. Reliable, dedicated funding to support research with the existing missions and to expand the astronomy small-satellite program will solidify Canada's trademark in space astronomy innovation., White paper identifier W054

We report improved masses, radii, and densities for four planets in two bright M-dwarf systems, K2-3 and GJ3470, derived from a combination of new radial velocity and transit observations. Supplementing K2 photometry with follow-up Spitzer transit observations refined the transit ephemerides of K2-3 b, c, and d by over a factor of 10. We analyze ground-based photometry from the Evryscope and Fairborn Observatory to determine the characteristic stellar activity timescales for our Gaussian Process fit, including the stellar rotation period and activity region decay timescale. The stellar rotation signals for both stars are evident in the radial velocity data and are included in our fit using a Gaussian process trained on the photometry. We find the masses of K2-3 b, K2-3 c and GJ3470 b to be 6.48$^{+0.99}_{-0.93}$, 2.14$^{+1.08}_{-1.04}$, and 12.58$^{+1.31}_{-1.28}$ M$_\oplus$ respectively. K2-3 d was not significantly detected and has a 3-$\sigma$ upper limit of 2.80 M$_\oplus$. These two systems are training cases for future TESS systems; due to the low planet densities ($\rho$ $, Comment: 21 pages, 11 figures, accepted to AJ

Since its launch in 2009, the Kepler telescope has found thousands of planets with radii between that of Earth and Neptune. Recent studies of the distribution of these planets have revealed a gap in the population near 1.5–2.0 R⊕, informally dividing these planets into "super-Earths" and "sub-Neptunes." The origin of this division is difficult to investigate directly because the majority of planets found by Kepler orbit distant, dim stars and are not amenable to radial velocity follow-up or transit spectroscopy, making bulk density and atmospheric measurements difficult. Here, we present the discovery and validation of a newly found 2.03^(+0.08)_(-0.07) R⊕ planet in direct proximity to the radius gap, orbiting the bright (J = 8.32 mag), nearby (D = 44.5 pc) high proper motion K3.5V star Wolf 503 (EPIC 212779563). We determine the possibility of a companion star and false positive detection to be extremely low using both archival images and high-contrast adaptive optics images from the Palomar observatory. The brightness of the host star makes Wolf 503b a prime target for prompt radial velocity follow-up, and with the small stellar radius (0.690 ± 0.025R⊙), it is also an excellent target for HST transit spectroscopy and detailed atmospheric characterization with JWST. With its measured radius near the gap in the planet radius and occurrence rate distribution, Wolf 503b offers a key opportunity to better understand the origin of this radius gap as well as the nature of the intriguing populations of "super-Earths" and "sub-Neptunes" as a whole.

We present a new Spitzer transit observation of K2–28b, a sub-Neptune (Rp = 2.45 ± 0.28 R⊕) orbiting a relatively bright (V_(mag) = 16.06, K_(mag) = 10.75) metal-rich M4 dwarf (EPIC 206318379). This star is one of only seven with masses less than 0.2 M⊙ known to host transiting planets, and the planet appears to be a slightly smaller analogue of GJ 1214b (2.85 ± 0.20 R⊕). Our new Spitzerobservations were taken two years after the original K2 discovery data and have a significantly higher cadence, allowing us to derive improved estimates for this planet's radius, semimajor axis, and orbital period, which greatly reduce the uncertainty in the prediction of near future transit times for the James Webb Space Telescope (JWST) observations. We also evaluate the system's suitability for atmospheric characterization with JWST and find that it is currently the only small (

We present a new {\em Spitzer} transit observation of K2$-$28b, a sub-Neptune ($R_{\rm p} = 2.45\pm0.28 R_{Earth}$) orbiting a relatively bright ($V_{\rm mag} = 16.06$, $K_{\rm mag} = 10.75$) metal-rich M4 dwarf (EPIC 206318379). This star is one of only seven with masses less than 0.2 M_{Sun} known to host transiting planets, and the planet appears to be a slightly smaller analogue of GJ 1214b ($2.85\pm0.20 R_{Earth}$; \citealt{2013A&A...549A..10H}). Our new {\em Spitzer} observations were taken two years after the original K2 discovery data and have a significantly higher cadence, allowing us to derive improved estimates for this planet's radius, semi-major axis, and orbital period, which greatly reduce the uncertainty in the prediction of near future transit times for the {\em James Webb Space Telescope} ({\em JWST}) observations. We also evaluate the system's suitability for atmospheric characterization with {\em JWST} and find that it is currently the only small (< 3 R_{Earth}) and cool ($< 600$ K) planet aside from GJ 1214b with a potentially detectable secondary eclipse. We also note that this system is a favorable target for near-infrared radial velocity instruments on larger telescopes (e.g., the Habitable Planet Finder on the Hobby-Eberly Telescope), making it one of only a handful of small, cool planets accessible with this technique. Finally, we compare our results with the simulated catalog of the Transiting Exoplanet Survey Satellite ({\em TESS}) and find K2$-$28b to be representative of the kind of mid-M systems that should be detectible in the {\em TESS} sample., 9 pages, 6 figures, accepted by AJ

The elemental compositions of hot Jupiters are informative relics of planet formation that can help us answer long-standing questions regarding the origin and formation of giant planets. Here, I present the main conclusions from a comprehensive atmospheric retrieval survey of eight hot Jupiters with detectable molecular absorption in their near-infrared transmission spectra. I analyze the eight transmission spectra using the newly-developed, self-consistent atmospheric retrieval framework, SCARLET. Unlike previous methods, SCARLET combines the physical and chemical consistency of complex atmospheric models with the statistical treatment of observational uncertainties known from atmospheric retrieval techniques. I find that all eight hot Jupiters consistently require carbon-to-oxygen ratios (C/O) below 0.9. The finding of C/O, Comment: under review at ApJ; updated to account for recently announced observations of WASP-12b and HD 209458b

The composition of a planet's atmosphere is determined by its formation, evolution, and present-day insolation. A planet's spectrum therefore may hold clues on its origins. We present a "chain" of models, linking the formation of a planet to its observable present-day spectrum. The chain links include (1) the planet's formation and migration, (2) its long-term thermodynamic evolution, (3) a variety of disk chemistry models, (4) a non-gray atmospheric model, and (5) a radiometric model to obtain simulated spectroscopic observations with James Webb Space Telescope and ARIEL. In our standard chemistry model the inner disk is depleted in refractory carbon as in the Solar System and in white dwarfs polluted by extrasolar planetesimals. Our main findings are: (1) envelope enrichment by planetesimal impacts during formation dominates the final planetary atmospheric composition of hot Jupiters. We investigate two, under this finding, prototypical formation pathways: a formation inside or outside the water iceline, called "dry" and "wet" planets, respectively. (2) Both the "dry" and "wet" planets are oxygen-rich (C/O < 1) due to the oxygen-rich nature of the solid building blocks. The "dry" planet's C/O ratio is 1 for the "dry" planet. (3) While we consistently find C/O ratios

Les atmosphères de Jupiter chaudes reçoivent des quantitées extrêmes de radiation de leur étoile hôte, ce qui nous permet d’étudier les processus chimiques et dynamiques d’atmosphères dans un régime d’énergie qui n’est pas accessible par l’étude du système solaire. La spectroscopie de transit et d’éclipse secondaire permet la caractérisation de ces atmosphères. Toutefois, ces méthodes ne considèrent pas la variation spatiale des abondances moléculaires, du profil de température et des nuages dans l’atmosphère. À l’aide de la méthode de cartographie par éclipse secondaire à plusieurs longueurs d’ondes, il est possible de mesurer la distribution spatiale des paramètres atmosphériques. À ce jour, cette méthode n’a été appliquée qu’à la Jupiter chaude HD 189733 b à partir d’observations photométriques du télescope spatial Spitzer à 8 μm. Avec le lancement prochain du JWST, des observations à haute précision spectrophotométrique sont attendues, ce qui renforce le besoin pour une méthode permettant la simulation et l’analyse statistique d’observations d’éclipse secondaire à plusieurs longueurs d’ondes. Nous présentons une nouvelle méthode afin de simuler des courbes de lumière à plusieurs longueurs d’ondes, ainsi qu’une méthode statistique pour déterminer la distribution atmosphérique à partir d’observations. La simulation des courbes de lumière à plusieurs longueurs d’ondes est discrétisée pour permettre le calcul rapide des modèles nécessaire à l’analyse statistique d’observations. Nous appliquons cette méthode à des observations simulées de JWST NIRSpec pour la planète WASP-33 b à diverses distributions spatiales de coefficient de dissociation de l’eau. Nos résultats indiquent que 5 observations d’éclipse secondaire sont suffisantes pour mesurer la distribution spatiale du coefficient de dissociation de l’eau en longitude et latitude. L’application de la méthode de cartographie par éclipse secondaire à plusieurs longueurs d’ondes va permettre d’appronfondir d’avantage notre connaissance des processus dynamiques des atmosphères de Jupiter chaudes., Hot Jupiter atmospheres, receiving extreme amounts of irradiation from their host star, enable us to study the atmospheric chemistry and dynamics of atmospheres at regimes that would otherwise be inaccessible from solar system observations. Transmission and emission spectroscopy of these atmospheres enables their characterization. However, these methods do not consider the spatial distribution of the molecular abundances, temperature profile, and clouds. Using multi-wavelength secondary eclipse mapping, it is possible to measure the spatial distribution of the atmospheric parameters. Secondary eclipse mapping has only been applied for photometric Spitzer/IRAC 8 μm observations of HD 189733 b so far. With the imminent launch of JWST, high-precision spectrophotometric observations of hot Jupiters are expected, reinforcing the need for a framework that can simulate and retrieve secondary eclipse mapping observations. We present a novel method to simulate secondary eclipse light curves for non-uniform atmospheres at multiple wavelengths, as well as a statistical method to retrieve the distribution from observations. The simulation of the multi-wavelength light curves is discretized to enable the fast computation necessary for statistical analysis of observations. We apply these methods to simulated JWST NIRSpec observations of WASP-33 b for various distributions of the water dissociation coefficient and conclude that 5 secondary eclipse observations are sufficient to constrain significant spatial variations in longitude and latitude. The application of the multi-wavelength secondary eclipse mapping to JWST will further deepen our understanding of the atmospheric dynamics processes to which hot Jupiter atmospheres are subjected.

Avec la découverte de milliers de nouvelles planètes au cours des vingt dernières années, une nouvelle population complexe de planètes plus petites que Neptune et plus grandes que la Terre a été découverte. Ces planètes se divisent en deux groupes : les plus grandes sub-Neptunes avec des atmosphères étendues dominées par H, et les plus petites super-Terres qui ont tout au plus des atmosphères minces. Cette division peut être expliquée par une variété de mécanismes, y compris la photoévaporation, la perte de masse alimentée par le noyau, et la formation de gaz pauvres et vides : la population de petites planètes est probablement façonnée par une combinaison de ces mécanismes qui peut dépendre du type stellaire. Dans ce travail, nous décrivons la découverte de deux nouvelles planètes qui sont bien adaptées à l'étude de la nature de la population des petites planètes : Wolf 503 b et LP 791-18 d. Wolf 503 b est une planète de \(2.03^{+0.08}_{-0.07} R_{\oplus}\) orbitant autour de l'étoile brillante (\(J=8.32\) mag), proche (\(D=44.5\) pc) à mouvement propre élevé K3.5V Wolf 503 (EPIC 212779563). Nous confirmons que la signature du transit K2 est planétaire en utilisant à la fois des images d'archives et des images d'optique adaptative à haut contraste de l'observatoire Palomar. Son rayon place Wolf 503b directement entre les populations de super-Terre et de sub-Neptune, un rayon auquel les planètes sont rarement trouvées et la composition de masse attendue est ambiguë, et la luminosité de l'étoile hôte fait de Wolf 503b une cible de choix pour le suivi des vitesses radiales et la spectroscopie de transit. La deuxième planète que nous présentons est une planète de taille terrestre orbitant autour de la naine froide M6 LP 791-18. La nouvelle planète d rejoint un système bien aligné avec au moins deux autres planètes, la plus externe étant une sous-Neptune, offrant une occasion unique à ce jour d'étudier un système avec une planète de taille terrestre tempérée et une sous-Neptune qui a conservé son enveloppe gazeuse ou volatile. La découverte de LP 791-18d permet de mesurer la masse du système grâce aux variations du temps de transit, et nous trouvons une masse de \( {9.3_{-1.4}^{+1.5}\,M_\oplus}\) pour la sub-Neptune LP 791-18c et une masse de \( {0.8_{-0.4}^{+0.5}\,M_\oplus}\) pour l'exo-Terre LP 791-18d (\({, With the discovery of thousands of new planets in the past twenty years, a new and complex population of planets has been discovered which are smaller than Neptune and larger than the Earth. These planets are split into two groups: the larger sub-Neptunes with extended H-dominated atmospheres, and the smaller super-Earths which have at most thin atmospheres. This division can be explained by a variety of mechanisms, including photoevaporation, core-powered mass-loss, and gas-poor and gas-empty formation: the small-planet population is likely shaped by a combination of these which may depend on stellar type. In this work we describe the discovery of two new planets which are well-suited to investigating the nature of the small planet population: Wolf 503b and LP 791-18d. Wolf 503 b is a \(2.03^{+0.08}_{-0.07} R_{\oplus}\) planet orbiting the bright (\(J=8.32\) mag), nearby (\(D=44.5\) pc) high proper motion K3.5V star Wolf 503 (EPIC 212779563). We confirm that the K2 transit signature is planetary using both archival images and high-contrast adaptive optics images from the Palomar observatory. Its radius places Wolf 503 b directly between the populations of super-Earths and sub-Neptunes, a radius at which planets are rarely found and the expected bulk composition is ambiguous, and the brightness of the host star makes Wolf 503b a prime target for radial velocity follow-up and transit spectroscopy. The second planet we introduce is an Earth-sized planet orbiting the cool M6 dwarf LP 791-18. The new planet d joins a well-aligned system with at least two more planets, the outermost being a sub-Neptune, providing a to-date unique opportunity to investigate a system with a temperate Earth-sized planet and a sub-Neptune that retained its gas or volatile envelope. The discovery of LP 791-18d makes the system amenable to mass measurements via transit timing variations, and we find a mass of \( {9.3_{-1.4}^{+1.5}\,M_\oplus}\) for the sub-Neptune LP 791-18c and a mass of \( {0.8_{-0.4}^{+0.5}\,M_\oplus}\) for the exo-Earth LP 791-18d (\( {

Le système TRAPPIST-1 offre une opportunité sans précédent de caractériser les premières planètes potentiellement habitables en dehors de notre système solaire. Dans ce mémoire est décrit le développement d’un pipeline de réduction de données personnalisé pour le mode WIRC+Spec de la caméra infrarouge à grand champ récemment mise à niveau à l’observatoire Palomar. Nous introduisons une nouvelle approche d’ajustement de la fonction d’étalement du point basée sur la transformation de Karhunen-Loève pour extraire des courbes de lumière photométrique et spectroscopique de sources de forme irrégulière, que nous appliquons aux observations de l’exoplanète TRAPPIST-1d pour mesurer ses spectres de transmission dans les bandes J (1.1 à 1.4 µm) et Ks (1.95 à 2.35 µm). Un guide détaillé est présenté pour l’implémentation d’un calcul de profils de température incluant l’équilibre radiatif et convectif pour une modélisation atmosphérique efficace et précise. En comparant une multitude de scénarios atmosphériques aux observations de TRAPPIST-1d, nous obtenons des contraintes sur la composition et la structure de son atmosphère, excluant les scénarios sans nuages avec des métallicités inférieures à 300 fois la valeur solaire à 3σ., The TRAPPIST-1 system provides an unprecedented opportunity to characterize the first potentially habitable planets outside our solar system. In this work we describe the development of a custom data reduction pipeline for the WIRC+Spec mode of the recently upgraded Wide Field Infrared Camera instrument on Palomar Observatory. We introduce a novel, Karhunen-Loève transform based approach to extract photometric and spectroscopic light curves from irregularly shaped sources, which we apply to observations of the TRAPPIST-1d exoplanet to measure the J band (1.1 to 1.4 µm) and Ks band (1.95 to 2.35 µm) transmission spectra. We also present a detailed guide into the implementation of a self-consistent, radiative-convective temperature structure calculation for efficient and accurate atmospheric modelling. Comparing a host of atmospheric scenarios to the observations of TRAPPIST-1d to date, we constrain its atmosphere, ruling out cloud-free atmospheres with metallicities lower than 300 times the solar value at 3σ confidence.