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WASP-17b

WASP-17b is a transiting orbiting the F-type star WASP-17, notable for its exceptionally large radius, low density, and orbital motion. Discovered in via the transit method by the (WASP) consortium, it completes an every 3.74 days at a semi-major axis of approximately 0.051 , placing it in a close-in that results in an equilibrium of around 1,700 K. With a of 0.49 masses and a radius of 1.83 radii, WASP-17b exhibits one of the lowest densities among known exoplanets at about 0.09 g/cm³, suggesting significant atmospheric inflation due to internal heating and stellar irradiation. The host star WASP-17 is an F4-type dwarf located approximately 406 parsecs away in the constellation , with an of about 6,500 K and a radius 1.3 times that of . WASP-17b's is inclined at nearly 87° to our , enabling precise observations, but it features a rare retrograde spin-orbit misalignment of -149°, indicating a likely dynamical history involving gravitational interactions with companion bodies. This misalignment was confirmed through spectroscopic measurements shortly after discovery. Atmospheric studies of WASP-17b have revealed a hydrogen- and helium-dominated envelope with evidence of water vapor and other molecules, observed via transmission spectroscopy with the Hubble Space Telescope. More recently, the James Webb Space Telescope (JWST) detected tiny quartz (SiO₂) crystals in the planet's clouds during a 2023 observation, marking the first identification of silicates in an exoplanet atmosphere and providing insights into high-temperature cloud formation processes. JWST observations in 2024 further measured a precise super-solar water abundance in the transmission spectrum and confirmed supersolar metallicity in the dayside atmosphere. The planet's dayside emission shows non-uniform temperatures, with JWST Mid-Infrared Instrument (MIRI) data indicating a cooler nightside and potential heat redistribution inefficiencies. These observations highlight WASP-17b as a key target for understanding the formation, evolution, and atmospheric dynamics of inflated gas giants.

Discovery and Nomenclature

Discovery

WASP-17b was discovered through the transit method as part of the (WASP) consortium survey and announced on August 11, 2009, via submission to by the discovery team. The planet was initially detected using photometric observations from the SuperWASP-South telescope array, which recorded 15,509 measurements of the host star between 2006 and 2008, identifying periodic dips in brightness indicative of a transiting . The discovery was led by David R. Anderson and a collaborative team from institutions including in the and the Geneva Observatory in . Confirmation followed through measurements obtained with the CORALIE spectrograph on the Euler 1.2 m at La Silla Observatory in , supplemented by high-precision spectra from the HARPS instrument on the ESO 3.6 m , which revealed the planet's orbital motion around the host star. These observations ruled out false positives and provided initial constraints on the system's parameters. The initial findings, including the first light curve analysis using Markov Chain Monte Carlo methods to model the transit and determine an orbital period of approximately 3.74 days, were detailed in a paper published in the Astrophysical Journal in 2010. Ground-based follow-up photometry was conducted at the South African Astronomical Observatory using the EulerCam on the Euler-Swiss telescope to confirm the transit depth and timing, ensuring the signal's consistency with a planetary transit. This discovery marked WASP-17b as the first exoplanet suggested to possess a retrograde orbit, opposite to the direction of its host star's rotation.

Nomenclature

WASP-17b received its provisional designation upon discovery, following the standard convention for exoplanets detected by the (WASP) survey, where the host star is numbered sequentially (WASP-17) and planets are lettered alphabetically starting with 'b' for the innermost or first confirmed. In December 2019, as part of the (IAU)'s centennial contest, the system was assigned to for public naming, resulting in the official approval of Ditsö̀ for the planet and Dìwö for the host star. These names derive from the of the indigenous Talamanca people in ; Dìwö means "," while Ditsö̀ refers to the name bestowed by the creator god Sibö̀ upon the first in Talamancan mythology, symbolizing reflection and origin. The IAU's exoplanet naming guidelines, established to promote global participation and , require that official names for exoplanets and their host stars form a thematic pair, draw from mythology, literature, or (preferring or lesser-known traditions), and avoid references to individuals, places, brands, or politically sensitive terms. This contest, held during the IAU's 100th anniversary, encouraged submissions from national organizing committees to foster international collaboration in astronomy and highlight underrepresented cultural narratives in celestial nomenclature.

Host Star

Characteristics

WASP-17 is classified as an F6V main-sequence star with an of 6550 ± 100 . Its mass is determined to be 1.20^{+0.10}{-0.11} M\sun, and its radius measures 1.38^{+0.20}{-0.18} R\sun. The star exhibits sub-solar , with an iron abundance of [Fe/H] = -0.25 ± 0.09. Isochrone fitting yields an estimated for WASP-17 of 3.0^{+0.9}_{-2.6} Gyr. The displays low chromospheric activity. WASP-17 shows moderate rotational broadening, with a projected equatorial of v \sin i = 9.0 ± 1.5 km s^{-1}, which corresponds to an expected period of approximately 8.5–11 days given the stellar .

Location and Visibility

The WASP-17 system is located in the constellation , at equatorial coordinates of 15ʰ 59ᵐ 51ˢ and −28° 03′ 42″ (J2000 epoch). It lies approximately 1,310 light-years (403 parsecs) from , a distance refined through measurements from the mission's Data Release 3 (2022). This places the system in a region of the southern celestial sky, accessible primarily to observers in the . The host star WASP-17 has an apparent visual of V = 11.6, rendering it faint enough to require mid-sized telescopes (typically 8–12 inches in ) for detailed observation under . Due to its southern , the system is best observed from latitudes south of 30° N, where it reaches higher altitudes and avoids horizon obstruction. Seasonal visibility peaks in the evening sky from to July for observers, when transits near midnight. In Galactic coordinates, WASP-17 resides at 346° and +19°, positioning it in the general direction of the and subject to moderate interstellar reddening along the . Observations account for an estimated E(B–V) reddening of about 0.05 magnitudes, which minimally affects photometric studies but is corrected for in spectral analyses.

Orbital Characteristics

Parameters

The orbital parameters of WASP-17b were determined primarily through analysis of photometric transit light curves and radial velocity measurements, providing key geometric elements of its orbit around the host star WASP-17. These parameters describe the size, shape, and orientation of the orbit, essential for modeling the planet's transit events and dynamical evolution. The values reflect refinements from multiple observations, confirming a close-in, short-period orbit typical of hot Jupiters.
ParameterValueSource
Orbital period (P)3.735485 ± 0.000002 days
Semi-major axis (a)0.05151 ± 0.00035
(e)< 0.020 (nearly circular)
Inclination (i)87.22° ± 0.14°
The near-circular (e < 0.020) implies minimal deviation from a perfect , consistent with tidal circularization over the 's lifetime. The high inclination of approximately 87.22° indicates an edge-on view from , enabling the detection of deep . Transit observations show a of approximately 4.4 hours and a depth of about 1.66% in visible light, reflecting the planet's large projected area relative to the star. The relationship between the and semi-major axis follows Kepler's third law, a^3 \propto P^2, scaled by the , which for WASP-17b yields the close-in separation of 0.05151 given the 3.7-day period. Additionally, the orbit is , with the planet moving opposite to the star's rotation, as inferred from the Rossiter-McLaughlin effect during transits.

Dynamics

WASP-17b orbits its host star in a direction, with a sky-projected spin-orbit misalignment angle of approximately 149°, as measured through observations of the Rossiter-McLaughlin effect. This effect, caused by the planet blocking portions of the rotating stellar disk during , distorts the signal and reveals the misalignment between the planet's and the star's equatorial plane. The measurement was obtained in 2010 using the HARPS spectrograph on the 3.6 m ESO telescope, confirming the retrograde nature independently from preliminary indications. The orbit exhibits long-term stability, attributed to its low (consistent with circular) and the absence of known additional planets in the system, which minimizes perturbations. As a with an of 3.7 days, WASP-17b resides close to its star without significant dynamical instabilities expected over planetary timescales. The suggests a complex history, where WASP-17b likely formed at a greater distance from its star—beyond the —and migrated inward through interactions such as planet-planet , which can induce large obliquities and reverse the orbital direction. This mechanism contrasts with standard disk-driven , which typically preserves , and aligns with dynamical models for misaligned . Tidal interactions between WASP-17b and its host star are expected to enforce strong , synchronizing the planet's rotation with its orbital motion due to the short and proximity. Additionally, these are expected to drive a gradual .

Physical Characteristics

Size and Mass

WASP-17b possesses a radius of 1.93 ± 0.05 radii, establishing it as one of the largest known exoplanets. This dimension was derived from the depth, quantified as (R_p / R_\star)^2, through analysis of photometric observations including Spitzer data combined with prior light curves via fitting. The planet's mass measures 0.48 ± 0.03 masses, obtained by fitting curves to yield the minimum mass m \sin i \approx \left( P K^3 / (2\pi G) \right)^{1/3}, where P is the and K is the semi-amplitude of approximately 0.053 km/s measured with the CORALIE and HARPS spectrographs. Since WASP-17b transits its host star, the inclination is near 90°, allowing the true mass to be approximated closely from this value. Uncertainties in both and arise primarily from assumptions in models applied to photometry and from stellar parameters, including the host star's (1.572 ± 0.056 radii) and (1.306 ± 0.026 masses), which propagate through the fitting process. Compared to , WASP-17b exhibits a substantially larger but lower , signifying an exceptionally low overall .

Density and Temperature

WASP-17b exhibits an exceptionally low of 0.09 ± 0.02 g/cm³, approximately 7% of 's of 1.33 g/cm³, signifying a highly inflated gaseous envelope that distinguishes it among known exoplanets. This value derives from and measurements yielding a of about 0.48 M_Jup and of roughly 1.93 R_Jup, resulting in a structure far less compact than typical gas giants. The low implies a puffed-up atmosphere, with the planet's consequently reduced to log g ≈ 2.7 (in cm/s² units), facilitating an extended that enhances signals and atmospheric observability. The planet's equilibrium temperature is approximately 1,770 , computed via the T_\mathrm{eq} = T_\star \sqrt{\frac{R_\star}{2 a}} (1 - A)^{1/4}, under assumptions of zero (A = 0) and full heat redistribution. Secondary observations reveal a hotter dayside of around 1,800 , reflecting intense stellar irradiation on the tidally locked facing hemisphere and a modest day-night , with recent JWST measurements indicating a cooler nightside around 1,000 . These thermal properties position WASP-17b at the boundary between hot and ultra-hot Jupiters, influencing its atmospheric dynamics. The of WASP-17b's arises primarily from radiative heating by its host star, which deposits into the upper atmosphere and, coupled with reduced opacity from molecular at high , prevents and sustains the expanded structure. Models indicate that about 70% of the absorbed stellar is redistributed across the , mitigating extreme temperature gradients while contributing to the overall bloating observed in low-gravity hot Jupiters like this one. This mechanism aligns with theoretical expectations for irradiated worlds, where internal cooling is inhibited by the insulating effect of the heated .

Atmosphere

Observations

The primary observational techniques for probing WASP-17b's atmosphere include transmission spectroscopy, which measures variations in transit depth across wavelengths to infer atmospheric absorption features, and emission spectroscopy, which analyzes contrasts during secondary eclipses to characterize thermal emission from the planet's dayside or nightside. Early atmospheric observations of WASP-17b were conducted using the Hubble Space Telescope's (WFC3) in 2013, employing transmission spectroscopy to detect faint signatures of in the near-infrared spectrum from 1.1 to 1.7 μm. This marked one of the first detections of molecular features in the planet's extended atmosphere, highlighting its hazy composition despite challenges from scattering. Ground-based efforts in the supplemented space-based data with near-infrared transit observations to refine the transmission . A tentative detection of sodium was reported in 2018 using high-resolution optical , suggesting potential presence, though subsequent analyses failed to confirm this feature. The (JWST) era began with (MIRI) low-resolution spectrometer observations in March 2023, yielding a transmission spanning 5–12 μm that resolved distinct opacity features, including a prominent signature at 8.6 μm. These data provided unprecedented mid-infrared coverage, revealing the influence of high-altitude clouds on the planet's atmospheric transmission. Subsequent JWST eclipse spectroscopy using the Near Infrared Imager and Slitless Spectrograph (NIRISS) single-object slitless (SOSS) mode in 2024 targeted the dayside from 0.8 to 5.3 μm, confirming a of approximately 1,400 K consistent with the planet's equilibrium temperature. This observation, analyzed in early 2025, demonstrated strong water absorption and supersolar on the dayside. In 2025, NIRSpec prism G395H observations further advanced nightside characterization through combined transit and eclipse measurements across 2.7–5.3 μm, employing phase-interpolated emission (PIE) techniques to isolate thermal contrasts and reveal chemical disequilibrium processes. These results, detailed in Gressier et al., highlighted heterogeneous and informed models of .

Composition

The atmosphere of WASP-17b features a composition dominated by molecular and , with significant enrichment in key trace gases and aerosols. (H₂O) has been detected at super-solar abundances, with retrieval analyses from near-infrared transmission yielding log(H₂O) ≈ -2.96, indicating an oxygen-rich environment consistent with enhanced volatile delivery during formation. The planet's is super-solar, exceeding 30 times levels based on dayside emission , which reflects high enrichment in heavy relative to . This is evidenced by oxygen-to-hydrogen (O/H) ratios with a 3σ lower limit greater than 3 times solar and a maximum likelihood estimate around 100 times solar, while carbon-to-hydrogen (C/H) ratios remain comparatively lower, contributing to an overall metal enhancement of approximately 10 times solar or more. The carbon-to-oxygen (C/O) ratio is sub-solar at ≈0.3 or below, signifying an oxygen-dominated chemistry that favors water and silicates over carbon-bearing species like . High-altitude hazes in the atmosphere consist of nanocrystalline (SiO₂) particles, approximately 0.01 μm in size, forming a reflective deck that scatters and absorbs mid-infrared at 8.6 μm. These clouds arise from in the hot, oxygen-rich upper layers and are shaped by strong equatorial winds exceeding 4 km/s (about 10,000 mph), which align the crystals and drive horizontal transport across the tidally locked planet. Atmospheric models for WASP-17b invoke at its high temperatures (around 1,800 K), where and thermal dissociation suppress formation in favor of and CO₂, though vertical mixing introduces disequilibrium effects by transporting deeper, metal-enriched gases upward. This low mean molecular weight, primarily from the H₂-He dominance despite elevated , supports the planet's extreme radius inflation by enhancing atmospheric opacity and heat retention.

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