Kepler-419c

Kepler-419c
Exoplanet List of exoplanets

Artist's impression of Kepler-419c (center), with a
hypothetical system of natural satellites orbiting around the planet.
Parent star
Star Kepler-419 (KOI-1474)
Constellation Cygnus
Right ascension (α) 19h 41m 40.3s
Declination (δ) +51° 11′ 05.15″
Apparent magnitude (mV) 13[1]
Distance2544 ly
(780[2] pc)
Spectral type F?V[3]
Mass (m) 1.39 (± 0.08)[3] M☉
Radius (r) 1.75 (± 0.08)[3] R☉
Temperature (T) 6430 (± 79)[3] K
Metallicity [Fe/H] 0.176 (± 0.07)[3]
Age 2.8 (± 1.3)[4] Gyr
Physical characteristics
Mass(m)7.3 (± 0.4)[3] MJ
Radius(r)~1.05 RJ
Stellar flux(F⊙)0.955[5] ⊕
Temperature (T) 250 K (−23 °C; −10 °F)
Orbital elements
Semi-major axis(a) 1.68 (± 0.03)[3] AU
Eccentricity (e) 0.184 (± 0.002)[3]
Orbital period(P) 675.47 (± 0.11)[3] d
Inclination (i) 88+3
−2[3]°
Discovery information
Discovery date 12 June 2014[3]
Discoverer(s) Kepler spacecraft
Discovery method Transit timing variations[3]
Discovery status Published
Other designations
KOI-1474.02, KIC 12365184 c, WISE J194140.29+511105.1 c, 2MASS J19414029+5111051 c
Database references
Extrasolar Planets
Encyclopaedia		data
SIMBADdata
Exoplanet Archivedata
Open Exoplanet Cataloguedata

Kepler-419c (also known by its Kepler Object of Interest designation KOI-1474.02) is a super-Jupiter exoplanet orbiting within the habitable zone of the star Kepler-419, the outermost of two such planets discovered by NASA's Kepler spacecraft. It is located about 2,544 light-years (780 parsecs, or nearly 2.4068×1016 km) from Earth in the constellation Cygnus.[3] The exoplanet was found by using the transit timing variation method, in which the variations of transit data from an exoplanet are studied to reveal a more distant companion.

Characteristics

Mass, radius and temperature

Kepler-419c is a super-Jupiter, an exoplanet that has a radius and mass greater than that of the planet Jupiter. It has a temperature of 250 K (−23 °C; −10 °F), somewhat cooler than the equilibrium temperature of the Earth.[5] It has a mass of 7.2 MJ, and a likely radius of around 1.05 RJ, based on its high mass.

Host star

The planet orbits an (F-type) star named Kepler-419. The star has a mass of 1.39 M☉ and a radius of 1.75 R☉. It has a surface temperature of 6430 K and is 2.8 billion years old. In comparison, the Sun is about 4.6 billion years old[6] and has a surface temperature of 5778 K.[7]

The star's apparent magnitude, or how bright it appears from Earth's perspective, is 12. It is too dim to be seen with the naked eye.

Orbit

Kepler-419c orbits its host star with 270% of the Sun's luminosity (2.7 L☉) about every 675 days (around 1.84 years) at a distance of 1.61 AU (compared to the orbital distance of Mars, which is 1.52 AU). It has a slightly eccentric orbit, with an eccentricity of 0.184. It receives about 95% of the amount of sunlight that Earth does.[5]

Habitability

Artist's impression of a habitable exomoon with liquid water and landmasses orbiting a gas giant.

Kepler-419c resides in the circumstellar habitable zone of the parent star. The exoplanet, with a mass of 7.28 MJ, is too massive to be rocky, and because of this the planet itself may not be habitable. However, Kepler-419c is listed as one of the candidates that may harbor potentially habitable moons, where, with the right atmospheric pressure and temperature, liquid water might exist on the surface of the moon.

For a stable orbit the ratio between the moon's orbital period Ps around its primary and that of the primary around its star Pp must be < 1/9, e.g. if a planet takes 90 days to orbit its star, the maximum stable orbit for a moon of that planet is less than 10 days.[8][9] Simulations suggest that a moon with an orbital period less than about 45 to 60 days will remain safely bound to a massive giant planet or brown dwarf that orbits 1 AU from a Sun-like star.[10] In the case of Kepler-419c, this would be practically the same to have a stable orbit, albeit a bit longer, around 65 days.

Tidal effects could also allow the moon to sustain plate tectonics, which would cause volcanic activity to regulate the moon's temperature[11][12] and create a geodynamo effect which would give the satellite a strong magnetic field.[13]

To support an Earth-like atmosphere for about 4.6 billion years (the age of the Earth), the moon would have to have a Mars-like density and at least a mass of 0.07 M⊕.[14] One way to decrease loss from sputtering is for the moon to have a strong magnetic field that can deflect stellar wind and radiation belts. NASA's Galileo's measurements hints large moons can have magnetic fields; it found that Jupiter's moon Ganymede has its own magnetosphere, even though its mass is only 0.025 M⊕.[10]

Discovery

In 2009, NASA's Kepler spacecraft was completing observing stars on its photometer, the instrument it uses to detect transit events, in which a planet crosses in front of and dims its host star for a brief and roughly regular period of time. In this last test, Kepler observed 50000 stars in the Kepler Input Catalog, including Kepler-419, the preliminary light curves were sent to the Kepler science team for analysis, who chose obvious planetary companions from the bunch for follow-up at observatories. Observations for the potential exoplanet candidates took place between 13 May 2009 and 17 March 2012. After observing the respective transits, the first planet, Kepler-419b, was announced.

Further investigations were made into the transit data of Kepler-419b, which was shown to be varying slightly, caused by a more distant orbiting planet. Data revealed that the responsible companion was about 7.3 times more massive than Jupiter and orbiting at a distance of 1.68 AU. The discovery was then announced on June 12, 2014.[3]

See also

References

  1. ↑ Kepler Mission Team (2009). "VizieR Online Data Catalog: Kepler Input Catalog (Kepler Mission Team, 2009)". VizieR On-line Data Catalog: V/133. Originally published in: 2009yCat.5133....0K. 5133. Bibcode:2009yCat.5133....0K.
  2. ↑ Dawson, Rebekah I.; Johnson, John Asher; Morton, Timothy D.; Crepp, Justin R.; Fabrycky, Daniel C.; Murray-Clay, Ruth A.; Howard, Andrew W. (2012). "The Photoeccentric Effect and Proto-hot Jupiters. II. KOI-1474.01, a Candidate Eccentric Planet Perturbed by an Unseen Companion". The Astrophysical Journal. 761 (2): 163. arXiv:1206.5579Freely accessible. Bibcode:2012ApJ...761..163D. doi:10.1088/0004-637X/761/2/163.
  3. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 Dawson, Rebekah I.; John Asher Johnson; Fabrycky, Daniel C.; Foreman-Mackey, Daniel; Murray-Clay, Ruth A.; Buchhave, Lars A.; Cargile, Phillip A.; Clubb, Kelsey I.; Fulton, Benjamin J.; Hebb, Leslie; Howard, Andrew W.; Huber, Daniel; Shporer, Avi; Valenti, Jeff A. (2014). "Large eccentricity, low mutual inclination: The three-dimensional architecture of a hierarchical system of giant planets". The Astrophysical Journal. 791 (2): 89. arXiv:1405.5229Freely accessible. doi:10.1088/0004-637X/791/2/89.
  4. ↑ "Notes for planet Kepler-419 c". The Extrasolar Planets Encyclopedia. Retrieved August 8, 2016.
  5. 1 2 3 http://www.hpcf.upr.edu/~abel/phl/hec_plots/hec_orbit/hec_orbit_Kepler-419_c.png
  6. ↑ Fraser Cain (16 September 2008). "How Old is the Sun?". Universe Today. Retrieved 19 February 2011.
  7. ↑ Fraser Cain (September 15, 2008). "Temperature of the Sun". Universe Today. Retrieved 19 February 2011.
  8. ↑ Kipping, David (2009). "Transit timing effects due to an exomoon". Monthly Notices of the Royal Astronomical Society. 392: 181–189. arXiv:0810.2243Freely accessible. Bibcode:2009MNRAS.392..181K. doi:10.1111/j.1365-2966.2008.13999.x. Retrieved 22 February 2012.
  9. ↑ Heller, R. (2012). "Exomoon habitability constrained by energy flux and orbital stability". Astronomy & Astrophysics. 545: L8. arXiv:1209.0050Freely accessible. Bibcode:2012A&A...545L...8H. doi:10.1051/0004-6361/201220003. ISSN 0004-6361.
  10. 1 2 Andrew J. LePage. "Habitable Moons:What does it take for a moon — or any world — to support life?". SkyandTelescope.com. Retrieved 2011-07-11.
  11. ↑ Glatzmaier, Gary A. "How Volcanoes Work – Volcano Climate Effects". Retrieved 29 February 2012.
  12. ↑ "Solar System Exploration: Io". Solar System Exploration. NASA. Retrieved 29 February 2012.
  13. ↑ Nave, R. "Magnetic Field of the Earth". Retrieved 29 February 2012.
  14. ↑ "In Search Of Habitable Moons". Pennsylvania State University. Retrieved 2011-07-11.

Coordinates: 19h 41m 40.3s, +51° 11′ 05.15″

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