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Giant Planet Formation by Gravitational Instability
Abstract
The recent discoveries of extrasolar giant planets, coupled with refined models of the compositions of Jupiter and Saturn, prompt a reexamination of theories of giant planet formation. An alternative to the favored core accretion hypothesis is examined here; gravitational instability in the outer solar nebula leading to giant planet formation. Three-dimensional hydrodynamic calculations of protoplanetary disks show that giant gaseous protoplanets can form with locally isothermal or adiabatic disk thermodynamics. Gravitational instability appears to be capable of forming giant planets with modest cores of ice and rock faster than the core accretion mechanism can.
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“An alternative planet formation model that has been hypothesized is that of gravitational instability (Zel'Dovich, 1970; Boss, 1997).”
From The Astrobiology Primer v2.0 (2016) · cites this paper as Boss, 1997
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The Galileo Probe: How it Has Changed Our Understanding of Jupiter
Young, R. (2003) · New Astronomy Reviews · doi:10.1016/s1387-6473(02)00272-5 · Cited by 60
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“…systems.6 Two main mechanisms for the formation of wide-orbit giant companions within protoplanetary disks have been suggested and explored: 1) top-down formation by gravitational disk instability (GI: e.g., Boss 1997), and 2) bottom-up formation by core accretion (CA: e.g., Pollack et al. 1996).”
BackgroundMeshkat, T., Mawet, D. P., Bryan, M. L., Hinkley, S., Bowler, B. P., Stapelfeldt, K. R., Batygin, K., Padgett, D., Morales, F. Y., Serabyn, E., et al. (2017) · The Astronomical Journal · doi:10.3847/1538-3881/aa8e9a · Cited by 80
“In contrast, the primary formation channel of more massive, distant bodies continues to be somewhat uncertain, since direct gravitational collapse (Boss 1997) remains a distinct possibility at large stello-centric radii, where the natal gaseous nebulae would have been comparatively colder.”
BackgroundMonnier, J., Harries, T., Aarnio, A., Adams, F., Andrews, S., Calvet, N., Espaillat, C., Hartmann, L., Hinkley, S., Kraus, S., et al. (2017) · doi:10.3847/1538-4357/aa6248 · Cited by 59
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BackgroundO'Donovan, F. T., Charbonneau, D., Torres, G., Mandushev, G., Dunham, E., Latham, D., Alonso, R., Brown, T., Esquerdo, G., Everett, M., et al. (2006) · The Astrophysical Journal · doi:10.1086/503740 · Cited by 59
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BackgroundPredicting Planets in Known Extrasolar Planetary Systems. III. Forming Terrestrial Planets
Raymond, S. N., Barnes, R., & Kaib, N. A. (2006) · The Astrophysical Journal · doi:10.1086/503594 · Cited by 83
“Indeed, several recent results have shown that giant planets may form in less than 1 Myr via either the bottom-up, core-accretion scenario (Rice & Armitage 2003; Alibert, Mordasini & Benz, 2004; Hubickyj et al. 2005) or the top-down, fragmentation scenario (Boss 1997; Mayer et al. , 2002).”
BackgroundPlanet Formation: Key Mechanisms and Global Models
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BackgroundThe Role of Magnetic Fields in the Formation of Protostellar Discs
Wurster, J., & Li, Z.-Y. (2018) · Frontiers in Astronomy and Space Sciences · doi:10.3389/fspas.2018.00039 · Cited by 58
“Later studies were radiative three-dimensional calculations that included simplified ideal magnetic fields calculations (e.g. Boss, 1997, 1999), or solved the complete MHD equations (e.g. Boss, 2002, 2005, 2007, 2009; Commerçon et al., 2010; Tomida et al., 2010, 2013; Bate et al., 2014).”
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“However, an alternative scenario for the formation of giant planets is the disk instability model (Boss, 1997, 2001), in which the giant planets form from the direct contraction of a gas clump resulting from local gravitational instability in the disk.”
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“The gravitational disc instability model for planet formation (e.g., Boss 1997) was thought to form planets only at distances greater than 50-100 AU (e.g., Rafikov 2005) due to inefficient cooling at closer distances (Gammie 2001; Mayer et al. 2004; Rafikov 2005; Meru & Bate 2011).”
BackgroundTesting Disk Instability Models for Giant Planet Formation
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“The disk instability mechanism for giant planet formation is based on the formation and survival of self-gravitating clumps of gas and dust in a marginally gravitationally unstable protoplanetary disk (Boss 1997; reviewed by Durisen et al. 2007).”
BackgroundSelf-citationALMA OBSERVATIONS OF THE DEBRIS DISK AROUND THE YOUNG SOLAR ANALOG HD 107146
Ricci, L., Carpenter, J. M., Fu, B., Hughes, A. M., Corder, S., & Isella, A. (2015) · The Astrophysical Journal · doi:10.1088/0004-637x/798/2/124 · Cited by 69
“This roughly corresponds to the mass limit for having gravitational instabilities in a disk around a 1 M⊙ star such as HD 107146 (e.g. Boss 1997; Rice et al. 2005).”
BackgroundA Determination of the Spin-Orbit Alignment of the Anomalously Dense Planet Orbiting HD 149026
Wolf, A., Laughlin, G., Henry, G., Fischer, D., Marcy, G., Butler, P., & Vogt, S. (2007) · The Astrophysical Journal · doi:10.1086/503354 · Cited by 57
“Unlike with core accretion theory, a metal-dominated composition is inconsistent with the gravitational instability mechanism for giant planet formation (e.g., Boss 1997, 2000, 2003).”
BackgroundThe Origin of Jovian Planets in Protostellar Disks: The Role of Dead Zones
Matsumura, S., & Pudritz, R. (2003) · doi:10.1086/378846 · Cited by 57
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BackgroundImportance of the accretion process in asteroid thermal evolution: 6 Hebe as an example
Ghosh, A., Weidenschilling, S., & McSween, H. (2003) · Meteoritics and Planetary Science · doi:10.1111/j.1945-5100.2003.tb00036.x · Cited by 57
Temperature Structures of Embedded Disks: Young Disks in Taurus Are Warm
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“For example, temperature determines whether the gas is susceptible to gravitational instabilities (see, e.g., a review by Kratter & Lodato 2016), a potential mechanism to form giant planets, stellar companions and accretion bursts (e.g., Boss 1997; Boley 2009; Vorobyov 2009; Tobin et al. 2016a).”
BackgroundNarang, M., Manoj, P., Furlan, E., Mordasini, C., Henning, T. K., Mathew, B., Banyal, R. K., & Sivarani, T. (2018) · The Astronomical Journal · doi:10.3847/1538-3881/aae391 · Cited by 73
“…of giant planets is that the Jupiters (MP ≤ 4MJ) are formed via core accretion whereas super-Jupiters (MP > 4MJ) are formed via the disk instability or the gravitational instability (e.g., Boss 1997; Rafikov 2005; Stamatellos & Whitworth 2008; Boley 2009; Cai et al. 2010; Boss 2010, 2011).”
BackgroundThe properties of planets around giant stars
Jones, M., Jenkins, J. S., Bluhm, P., Rojo, P., & Melo, C. (2014) · doi:10.1051/0004-6361/201323345 · Cited by 56
“On the other hand, giant planets around intermediate-mass stars might be efficiently formed by the disk instability mechanism (Boss 1997).”
BackgroundPLANETARY AND OTHER SHORT BINARY MICROLENSING EVENTS FROM THE MOA SHORT-EVENT ANALYSIS
Bennett, D. P., Sumi, T., Bond, I., Kamiya, K., Abe, F., Botzler, C., Fukui, A., Furusawa, K., Itow, Y., Korpela, A., et al. (2012) · The Astrophysical Journal · doi:10.1088/0004-637x/757/2/119 · Cited by 56
“Alternatively, distant bound planets could have formed in situ by gravitational instability (Boss 1997).”
BackgroundIkoma, M., Guillot, T., Genda, H., Tanigawa, T., & Ida, S. (2006) · The Astrophysical Journal · doi:10.1086/507088 · Cited by 100
“As noted by Sato et al. (2005), such a big core points toward formation of the planet in the core accretion scenario (e.g., Mizuno 1980; Bodenheimer & Pollack 1986), rather than in the disk instability scenario (e.g., Boss 1997).”
BackgroundPlanetesimal capture in the disk instability model
Helled, R., Podolak, M., & Kovetz, A. (2006) · doi:10.1016/j.icarus.2006.06.011 · Cited by 55
“Such clumps can contract to form giant gaseous protoplanets (Boss 1997; Boss 1998b).”
BackgroundSheehan, P., Tobin, J., Federman, S., Megeath, S., & Looney, L. (2020) · Astrophysical Journal · doi:10.3847/1538-4357/abbad5 · Cited by 54
“Gravitational instabilities in disks could potentially form planets on significantly shorter timescales than core accretion (e.g. Boss 1997; Durisen et al. 2007; Boss 2011), and could therefore explain how these features are seen at such early times.”
BackgroundHan, C., Jung, Y., Udalski, A., Sumi, T., Gaudi, B., Gould, A., Bennett, D., Tsapras, Y., Szymański, M., Kubiak, M., et al. (2013) · doi:10.1088/0004-637x/778/1/38 · Cited by 54
“Therefore, it seems unlikely that these companions formed from the protoplanetary disk material via either of the popular gi nt planet formation mechanisms of core accretion (Pollack et al. 1996) or disk fragmentation (Kuiper 1951; Cameron 1978; Boss 1997; Durisen et al. 2007).”
BackgroundTHE FIRST PLANETS: THE CRITICAL METALLICITY FOR PLANET FORMATION
Johnson, J. L., & Li, H. (2012) · The Astrophysical Journal · doi:10.1088/0004-637x/751/2/81 · Cited by 90
“…AU; e.g., Lafrenière et al. 2008, 2011; Biller et al. 2011; Ireland et al. 2011) may already pose a challenge to the core accretion model, and it has been suggested that the gravitational instability model (e.g., Boss 1997) may better explain their formation (e.g., Dodson-Robinson et al. 2009).”
BackgroundTIDALLY INDUCED BROWN DWARF AND PLANET FORMATION IN CIRCUMSTELLAR DISKS
Thies, I., Kroupa, P., Goodwin, S., Stamatellos, D., & Whitworth, A. (2010) · The Astrophysical Journal · doi:10.1088/0004-637x/717/1/577 · Cited by 54
“Fragmentation has been proposed as an alternative way to form the most massive gas giant planets by Mayer et al. (2002); Boss (1997, 2004, 2006).”
BackgroundON THE POSSIBILITY OF ENRICHMENT AND DIFFERENTIATION IN GAS GIANTS DURING BIRTH BY DISK INSTABILITY
Boley, A., & Durisen, R. H. (2010) · Proceedings of the International Astronomical Union · doi:10.1088/0004-637x/724/1/618 · Cited by 54
“Core accretion (e.g., Pollack et al. 1996; Hubickyj et al. 2005) and direct formation by disk instability (e.g., Cameron 1978; Boss 1997, 1998) are both viable modes of gas giant planet formation and both may be required to explain the diversity of observed planetary systems.”
BackgroundMetallicity of the massive protoplanets around HR 8799 If formed by gravitational instability
Helled, R., & Bodenheimer, P. (2009) · Icarus · doi:10.1016/j.icarus.2009.11.023 · Cited by 54
“, 2005), in the gravitational instability model (Cameron, 1978; Boss, 1997) the planet’s enrichment with solids is so far considered as an independent part of the actual formation mechanism.”
BackgroundMethodInfluentialThe effects of opacity on gravitational stability in protoplanetary discs
Cossins, P., Lodato, G., & Clarke, C. J. (2009) · Monthly Notices of the Royal Astronomical Society · doi:10.1111/j.1365-2966.2009.15835.x · Cited by 80
“In protoplanetary discs where the self-gravity of the gas is dynamically important, direct gravitational collapse of locally Jeans-unstable over-densities within the disc (Boss, 1997Boss, 1998Durisen et al., 2007) would also produce giant planets very rapidly, on the local dynamical timescale.”
BackgroundKortenkamp, S. J. (2000) · Icarus · doi:10.1006/icar.1999.6241 · Cited by 55
Raymond, S. (2006) · The Astrophysical Journal · doi:10.1086/505596 · Cited by 52
“Thus, we consider our simulations a reasonable approximation of terrestrial accretion even if giant planets form more quickly than embryos (e.g., Boss 1997).”
BackgroundPlanetesimals to brown dwarfs: What is a planet?
Basri, G., & Brown, M. E. (2006) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.34.031405.125058 · Cited by 52
“The main competition to the standard model comes from “rapid collapse” scenarios, which posit that disks that are cool and massive enough can form gas giants directly through gravitational instabilities (Boss 1997).”
BackgroundIs there an exoplanet in the solar system?
Mustill, A. J., Raymond, S. N., & Davies, M. B. (2016) · Monthly Notices of the Royal Astronomical Society: Letters · doi:10.1093/mnrasl/slw075 · Cited by 52
“While in situ formation of super-Jovian planets may be possible via gravitational instability (Boss 1997; Kratter & Lodato 2016), this could not lead to the formation of Neptune-or super Earth-mass planets.”
A Stellar Mass Dependence of Structured Disks: A Possible Link with Exoplanet Demographics
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Perryman, M. A. C. (2011) · Cambridge University Press eBooks · doi:10.1017/cbo9780511994852.011 · Cited by 71
Heavy Metal Rules. I. Exoplanet Incidence and Metallicity
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“, [53,261], GI/TD model of Nayakshin [61] can also explain the formation of low-mass planets.”
BackgroundThermodynamics of giant planet formation: shocking hot surfaces on circumplanetary discs
Szulágyi, J., & Mordasini, C. (2016) · doi:10.1093/mnrasl/slw212 · Cited by 50
“Giant planets are thought to form either via core-accretion (Pollack et al. 1996) or gravitational instability scenario (Boss 1997).”
BackgroundThe formation and habitability of terrestrial planets in the presence of close-in giant planets
Raymond, S. N., Quinn, T., & Lunine, J. I. (2005) · Icarus · doi:10.1016/j.icarus.2005.03.008 · Cited by 81
Formation, Orbital and Internal Evolutions of Young Planetary Systems
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“4.2: it constrains the physics of gas accretion and potentially even the mode of formation, namely core accretion (Perri and Cameron 1974; Mizuno 1980; Bodenheimer and Pollack 1986) or gravitational instability (Toomre 1981; Boss 1997; Durisen et al. 2007).”
BackgroundInfluentialAnglada-Escud'e, G., Boss, A., Weinberger, A., Thompson, I., Butler, R. P., Vogt, S., & Rivera, E. (2011) · doi:10.1088/0004-637x/746/1/37 · Cited by 48
“The competing mechanism model for planet formation (Boss 1997, disk instability model) should not be very sensitive to the metallicity of the host star, so this has also been suggested as evidence in favor the core-accretion scenario (e.g., see Ida & Lin 2004; Mordasini et al. 2009).”
BackgroundSelf-citationNumerical convergence in self-gravitating disc simulations: initial conditions and edge effects
Paardekooper, S.-J., Baruteau, C., & Meru, F. (2011) · Monthly Notices of the Royal Astronomical Society Letters · doi:10.1111/j.1745-3933.2011.01099.x · Cited by 68
“The determination of the critical value of β is important in models of giant planet formation that rely on disc instability (e.g. Boss 1997; Boley et al. 2010).”
BackgroundSozzetti, A. (2004) · doi:10.1111/j.1365-2966.2004.08281.x · Cited by 48
“…stage to make meaningful statements on the relative roles of the two proposed mechanisms for gas giant planet formation, i.e. core accretion (e.g. Lissauer 1993; Pollack et al. 1996; Alibert, Mordasini & Benz 2004) and disc instability (e.g. Boss 1997, 2001; Mayer et al. 2002; Rice et al. 2003).”
BackgroundProtostellar Disk Instabilities and the Formation of Substellar Companions
Pickett, B., Durisen, R. H., Cassen, P., & Mejía, A. C. (2000) · doi:10.1086/312884 · Cited by 48
“In particular, positive nonrotational velocities are severely damped for numerical stability in Boss (1997, 1998).”
BackgroundMethodResultInfluentialEvidence for a Vertical Dependence on the Pressure Structure in AS 209
Teague, R., Bae, J., Birnstiel, T., & Bergin, E. (2018) · Astrophysical Journal · doi:10.3847/1538-4357/aae836 · Cited by 47
“Dynamical time scales at these radii are prohibitive for core formation and the formation of planets, although planet formation via gravitational instability is a possibility (Boss 1997).”
BackgroundCavalié, T., Vénot, O., Selsis, F., Hersant, F., Hartogh, P., & Leconte, J. (2017) · Icarus · doi:10.1016/j.icarus.2017.03.015 · Cited by 53
“E P] 1 regarding the formation of giant planets: disk gravitational instability (Boss, 1997) and core accretion (Pollack et al., 1996).”
BackgroundMethodInfluentialLAPLACE: A mission to Europa and the Jupiter System for ESA’s Cosmic Vision Programme
Blanc, M., Alibert, Y., André, N., Atreya, S. K., Beebe, R. F., Benz, W., Bolton, S. J., Coradini, A., Coustenis, A., Dehant, V., et al. (2009) · Experimental Astronomy · doi:10.1007/s10686-008-9127-4 · Cited by 44
“The second scenario [8, 52] assumes that giant planets are formed by gravitational instabilities in the massive proto-Solar Nebula [7], leading to the rapid formation of density enhancements—or clumps—with solar chemical compositions and masses probably larger than the present ones of the giant planets.”
BackgroundDust accretion onto high-mass planets
Paardekooper, S. (2006) · doi:10.1051/0004-6361:20066326 · Cited by 47
“The alternative for the core accretion model is the gravitational instability scenario, in which a massive disk becomes gravitational unstable and fragments into giant planets (Boss 1997; Mayer et al. 2004).”
BackgroundFormation of gas and ice giant planets
Boss, A. P. (2002) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(02)00808-7 · Cited by 42
Self-citationBae, J., Teague, R., Andrews, S., Benisty, M., Facchini, S., Galloway-Sprietsma, M., Loomis, R., Aikawa, Y., Alarcón, F., Bergin, E., et al. (2022) · Astrophysical Journal Letters · doi:10.3847/2041-8213/ac7fa3 · Cited by 46
“One possibility is that the AS 209 disk was gravitationally unstable in the past and the planet formed via gravitational instability (GI; Boss 1997).”
BackgroundSIGNATURES OF GRAVITATIONAL INSTABILITY IN RESOLVED IMAGES OF PROTOSTELLAR DISKS
Dong, R., Vorobyov, E. I., Pavlyuchenkov, Y. N., Chiang, E., & Liu, H. B. (2016) · The Astrophysical Journal · doi:10.3847/0004-637x/823/2/141 · Cited by 69
“…orbital distances from the star, disk fragmentation may form bound objects such as giant planets, brown dwarfs, or stellar mass companions (e.g., Boss 1997; Rice et al. 2005; Rafikov 2005; Stamatellos & Whitworth 2009; Kratter et al. 2010; Meru & Bate 2011; Machida et al. 2011b; Vorobyov & Basu…”
BackgroundThebault, P., & Haghighipour, N. (2014) · Springer eBooks · doi:10.1007/978-3-662-45052-9_13 · Cited by 46
“This single-star-environment tropism does also affect the alternative planet-forming scenario by gravitational instabilities (Boss, 1997), which has witnessed a renewed interest after the discovery of jovian exoplanets at large radial distances from their star (Boss, 2011).”
BackgroundInfluentialDeep Exploration of the Planets HR 8799 b, c, and d with Moderate-resolution Spectroscopy
Ruffio, J., Konopacky, Q., Barman, T., Macintosh, B., Hoch, K., de Rosa, R. D., Wang, J. J., Czekala, I., & Marois, C. (2021) · Astronomical Journal · doi:10.3847/1538-3881/ac273a · Cited by 45
“There are two main pathways to form substellar companions around young stars (Lissauer 1987; Boss 1997; Boley 2009).”
BackgroundBonnefoy, M., Perraut, K., Lagrange, A. ‐., Delorme, P., Vigan, A., Line, M. R., Rodet, L., Ginski, C., Mourard, D., Marleau, G.-D., et al. (2018) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201832942 · Cited by 78
“The gravitational instability scenario (hereafter GI; e.g., Boss 1997; Forgan & Rice 2013) has been proposed as an alternative to solve that issue.”
BackgroundSzulágyi, J., Mayer, L., & Quinn, T. (2016) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stw2617 · Cited by 45
“The two widely accepted planet formation theories, core accretion (Pollack et al. 1996) and gravitational instability (Boss 1997) both predict that circumplanetary disks form around giant planets (e.g. Quillen & Trilling 1998; Canup & Ward 2002; Ward & Canup 2010).”
BackgroundSOLUBILITY OF IRON IN METALLIC HYDROGEN AND STABILITY OF DENSE CORES IN GIANT PLANETS
Wahl, S., Wilson, H., & Militzer, B. (2013) · The Astrophysical Journal · doi:10.1088/0004-637x/773/2/95 · Cited by 45
“A competing theory involves collapse of a region of the disk under self-gravity, e.g. (Boss 1997), but may have difficulty explaining significant enrichment of refractory elements (Hubbard et al. 2002; Guillot 2005).”
BackgroundCrepp, J., & Johnson, J. (2011) · The Astrophysical Journal · doi:10.1088/0004-637x/733/2/126 · Cited by 45
“One currently favored explanation is that core-accretion and other processes related to gravitational disk instabilities are responsible for building each group respectively (Pollack et al. 1996; Ida and Lin 2004; Boss 1997; Durisen et al. 2007).”
BackgroundTHE GROWTH AND MIGRATION OF JOVIAN PLANETS IN EVOLVING PROTOSTELLAR DISKS WITH DEAD ZONES
Matsumura, S., Pudritz, R. E., & Thommes, E. W. (2009) · The Astrophysical Journal · doi:10.1088/0004-637x/691/2/1764 · Cited by 52
“Since this is uncomfortably close to a typical disk life time, it was considered as one of the weakest points of core accretion scenario (e.g. Boss 1997).”
BackgroundMultiple Spiral Arms in the Disk around Intermediate-mass Binary HD 34700A
Monnier, J., Harries, T., Bae, J., Setterholm, B., Laws, A., Aarnio, A., Adams, F., Andrews, S., Calvet, N., Espaillat, C., et al. (2019) · Astrophysical Journal · doi:10.3847/1538-4357/aafe87 · Cited by 44
“Observations are needed to determine the importance of effects such as gravitational instability (Boss 1997), streaming instability (Johansen et al. 2007), dust growth (Birnstiel et al. 2010), core accretion (Pollack et al. 1996), planetary migration (Tanaka et al. 2002), and more.”
BackgroundExoplanets beyond the Solar neighbourhood: Galactic tidal perturbations
Veras, D., & Evans, N. (2012) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/sts647 · Cited by 44
“Dodson-Robinson et al. (2009) claim that 35 AU is a rough limit beyond which massive gas giant planets must form by an alternate mechanism, such as gravitational instability in the disc (e.g. Cameron 1978; Boss 1997); Boley (2009) claims that this limit is approximately 100 AU.”
BackgroundAbsil, O., & Mawet, D. (2009) · The Astronomy and Astrophysics Review · doi:10.1007/s00159-009-0028-y · Cited by 44
“A completely different formation mechanism for gas giant, based on direct gravitational collapse of young protoplaneraty discs, has also been proposed (Boss 1997).”
BackgroundNero, D., & Bjorkman, K. S. (2009) · The Astrophysical Journal · doi:10.1088/0004-637x/702/2/l163 · Cited by 69
“Another mechanism for giant planet formation is disk fragmentation as a consequence of the gravitational instability (Kuiper 1951; Cameron 1978; Boss 1997, see also the recent review by Durisen et al. 2007 and Stamatellos & Whitworth Electronic address: dnero@physics.utoledo.edu 2009 for recent…”
BackgroundDead zones and extrasolar planetary properties
Matsumura, S., & Pudritz, R. (2005) · doi:10.1111/j.1365-2966.2005.09737.x · Cited by 44
“Regarding the third point, the mass accumulation at the edge of a dead zone, or even at the edge of a gap opened by a planet, may lead to planet formation via gravitational instability, which requires a dense, cold region (e.g. Boss 1997; Mayer et al. 2002).”
BackgroundBeyond the Principle of Plentitude: A Review of Terrestrial Planet Habitability
Gaidos, E. J., Deschenes, B., Dundon, L., Fagan, K., Menviel, L., Moskovitz, N., & Workman, M. (2005) · Astrobiology · doi:10.1089/ast.2005.5.100 · Cited by 46
“This would be an issue giant planets rapidly formed via a mechanism (Boss, 1997) but not if formed around a slowly accreting Mizuno, 1980).”
Mass Loss and Jet Outflow in the Orion Nebula Proplyd LV 2
Henney, W., O'Dell, C., Meaburn, J., Garrington, S., & López, J. (2002) · doi:10.1086/338055 · Cited by 44
“Boss (1997) has argued that planet formation could occur gravitationally in some circumstances in timescales of about 103 yr, whereas the accretion onto a rocky core process (Pollack et al. 1996) would require 106È107 yr ; i.e., we cannot come to a conclusion on the viability of planet formation…”
BackgroundThompson, T. A. (2013) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stt102 · Cited by 48
“Gas- and ice-giant planets may also form by gravitational instability (Boss 1997, 2000; Pickett et al. 2003; Durisen et al. 2007).”
BackgroundPOST-CAPTURE EVOLUTION OF POTENTIALLY HABITABLE EXOMOONS
Porter, S., & Grundy, W. (2011) · The Astrophysical Journal Letters · doi:10.1088/2041-8205/736/1/l14 · Cited by 43
“Current giant-planet formation models assume that they are created at distances beyond the stability point of ice (e.g. Lissauer 1987; Boss 1997), which implies conditions not suitable to surface habitability.”
BackgroundKramm, U., Nettelmann, N., Redmer, R., & Stevenson, D. J. (2010) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201015803 · Cited by 59
“Knowledge about the core masses of planets is highly desired because it is thought to help to distinguish between the possible planet formation scenarios of core accretion (see e.g. Pollack et al. 1996) and gravitational instability (see e.g. Boss 1997).”
BackgroundLONG-PERIOD EXOPLANETS FROM DYNAMICAL RELAXATION
Scharf, C. A., & Kristen Menou, A. (2009) · The Astrophysical Journal · doi:10.1088/0004-637x/693/2/l113 · Cited by 73
“The two leading scenarios for planet formation, core accretion and direct gravitational collapse, should lead to signif- icantly different initial orbital outcomes for young planets (e.g., Lissauer 1993; Boss 1997; Papaloizou & Terquem 2006).”
BackgroundIrregular Satellites in the Context of Planet Formation
Jewitt, D., & Sheppard, S. (2004) · Springer eBooks · doi:10.1007/1-4020-4038-5_22 · Cited by 43
“To explain the ice giants Uranus and Neptune, Boss (2003) has advocated a model in which these planets are the remnants of ∼2 MJ gas giants ablated by a sustained ionizing flux of photons from nearby OB type stars.”
BackgroundColloquium: Stars, planets, and metals
GONZÁLEZ, G. A. (2003) · Reviews of Modern Physics · doi:10.1103/revmodphys.75.101 · Cited by 72
Jupiter formed as a pebble pile around the N2 ice line
Bosman, A. D., Cridland, A. J., & Miguel, Y. (2019) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201936827 · Cited by 73
“Present address: Department of Astronomy, University of Michigan, 311 West Hall, 1085 S. University Avenue, Ann Arbor, MI 48109, USA gions of the solar nebula, before migrating in (Boss 1997, 2002; Boley et al. 2010).”
BackgroundThe Fragmentation Criteria in Local Vertically Stratified Self-gravitating Disk Simulations
Baehr, H., Klahr, H., & Kratter, K. M. (2017) · The Astrophysical Journal · doi:10.3847/1538-4357/aa8a66 · Cited by 52
“Fragmentation through gravitational instability (GI) is a model which forms stellar companions quickly and typically only works in the cool outer reaches of the circumstellar disk (Kuiper, 1951; Boss, 1997).”
BackgroundDahm, S. (2005) · The Astronomical Journal · doi:10.1086/433178 · Cited by 42
“If, however, inner disks dissipate rapidly on the order of 1 Myr, the disk instability mechanism proposed by Boss (1997) may be required to explain these subAU gas giants.”
BackgroundThe frequency of giant planets around metal-poor stars
Mortier, A., Santos, N. C., Sozzetti, A., Mayor, M., Latham, D. W., Bonfils, X., & Udry, S. (2012) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201118651 · Cited by 67
“…et al. 2004), where gas from the protoplanetary disk is accreted around a previously formed rocky/icy core, and the disk instability model (e.g. Boss 1997; Mayer et al. 2002), where a planet is formed ⋆ The data presented herein are based on observations collected at the La Silla Parana…”
MethodTHE HEAVY-ELEMENT COMPOSITION OF DISK INSTABILITY PLANETS CAN RANGE FROM SUB- TO SUPER-NEBULAR
Boley, A., Helled, R., & Payne, M. (2011) · The Astrophysical Journal · doi:10.1088/0004-637x/735/1/30 · Cited by 41
“Core accretion plus gas capture (e.g., Pollack et al. 1996) and direct formation by disk instability (e.g., Cameron 1978; Boss 1997, 1998) are both viable formation models for gas giant planets (see D’Angelo et al. 2010 for a review).”
BackgroundInfluentialSpiral shocks in the accretion disc of IP Peg during outburst maximum
Harlaftis, E. T., Steeghs, D., Horne, K., Martín, E., & Magazzú, A. (1999) · Monthly Notices of the Royal Astronomical Society · doi:10.1046/j.1365-8711.1999.02502.x · Cited by 51
“Moreover, spiral shocks have been found in simulations of protosolar discs, and have been proposed as a means of converting the gaseous protostellar disc into orbiting planetesimals (Boss 1997).”
BackgroundGalvagni, M., Hayfield, T., Boley, A., Mayer, L., Roskar, R., & Saha, P. (2012) · Monthly Notices of the Royal Astronomical Society · doi:10.1111/j.1365-2966.2012.22096.x · Cited by 40
“Renewed interest in disc instability as a planet-forming mechanism is largely due to the advancement of Boss (1997) and to recent discoveries of extrasolar planets c© 0000 RAS ar X iv :1 20 9.”
BackgroundFormation of terrestrial planet cores inside giant planet embryos
Nayakshin, S. (2011) · Monthly Notices of the Royal Astronomical Society · doi:10.1111/j.1365-2966.2011.18230.x · Cited by 69
“Boss (1997) argued that giant planets may form this way.”
BackgroundDirect imaging of sub-Jupiter mass exoplanets with James Webb Space Telescope coronagraphy
Carter, A. L., Hinkley, S., Bonavita, M., Phillips, M. W., Girard, J. H., Perrin, M. D., Pueyo, L. A., Vigan, A., Gagné, J., & Skemer, A. J. I. (2020) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/staa3579 · Cited by 41
“Furthermore, both core accretion (Pollack et al. 1996) and gravitational insta- MNRAS 000, 1–18 (2020) bility (Boss 1997) population synthesis models have shown that at separations beyond 50 au, where JWST is most sensitive, planetarymass companions are increasingly uncommon (Forgan&Rice 2013;…”
BackgroundEarth-like habitats in planetary systems
Fritz, J., Bitsch, B., Kührt, E., Morbidelli, A., Tornow, C., Wünnemann, K., Fernandes, V. A., Grenfell, J. L., Rauer, H., Wagner, R., et al. (2014) · Planetary and Space Science · doi:10.1016/j.pss.2014.03.003 · Cited by 38
“Indeed, massive disks can become gravitationally unstable in their outer parts, which can trigger giant planet formation through gravitational collapse (Boss, 1997).”
BackgroundCai, K., Pickett, M. K., Durisen, R. H., & Milne, A. M. (2010) · The Astrophysical Journal Letters · doi:10.1088/2041-8205/716/2/l176 · Cited by 43
“…the disk instability mechanism, where gas-phase gravitational instabilities (GI’s) produce spiral waves that fragment into protoplanetary clumps (Boss 1997, 1998, 2000, 2001, 2002, 2003, 2004, 2005, 2007, 2009; Pickett et al. 1998, 2000a,b, 2003; Nelson et al. 1998, 2000; Nelson 2006; Gammie…”
BackgroundStarspot-Induced Radial Velocity Variability in LkCa 19
Huerta, M., Johns-Krull, C., Prato, L., Hartigan, P., & Jaffe, D. (2007) · doi:10.1086/526415 · Cited by 38
“Since the timescale for the core accretion model (Pollack et al. 1996) is longer than formation due to disk instability (Boss 1997), a detection of a young planet around a T Tauri star should also provide clues to the formation mechanism itself.”
BackgroundImplications of Extrasolar Planets for Understanding Planet Formation
Bodenheimer, P. H., & Lin, D. N. C. (2002) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.30.091201.140357 · Cited by 46
Microlensing events indicate that super-Earth exoplanets are common in Jupiter-like orbits.
Zang, W., Jung, Y., Yee, J., Hwang, K., Yang, H.-J., Udalski, A., Sumi, T., Gould, A., Mao, S., Albrow, M., et al. (2025) · Science · doi:10.1126/science.adn6088 · Cited by 37
A dust and gas cavity in the disc around CQ Tau revealed by ALMA
Gabellini, M. U., Miotello, A., Facchini, S., Ragusa, E., Lodato, G., Testi, L., Benisty, M., Bruderer, S., Kurtovic, N., Andrews, S., et al. (2019) · Monthly notices of the Royal Astronomical Society · doi:10.1093/mnras/stz1138 · Cited by 37
“The main scenarios currently considered for planet formation are the core accretion model (e.g. Pollack et al. 1996) and disc instability (e.g. Boss 1997).”
BackgroundSurvival rates of planets in open clusters: the Pleiades, Hyades, and Praesepe clusters
Fujii, M. S., & Hori, Y. (2019) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201834677 · Cited by 46
“However, the birthplace of planets are expected to be inside several 10AU both in the core-accretion model (e.g., Pollack et al. 1996) and in the disk instability scenario (e.g., Boss 1997).”
BackgroundThe properties of discs around planets and brown dwarfs as evidence for disc fragmentation
Stamatellos, D., & Herczeg, G. (2015) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stv526 · Cited by 37
“…& Nordlund 2004; Hennebelle E-mail: dstamatellos@uclan.ac.uk & Chabrier 2008, 2009; Hopkins 2013), (ii) by fragmentation of protostellar discs (Boss 1997; Stamatellos, Hubber & Whitworth 2007a; Attwood et al. 2009; Boley 2009; Stamatellos & Whitworth 2009a), which may not even be…”
BackgroundCosmochemical consequences of particle trajectories during FU Orionis outbursts by the early Sun
Boss, A., Alexander, C. M. O. '., & Podolak, M. (2012) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2012.06.046 · Cited by 37
“The alternative formation mechanism, disk instability (Boss, 1997), seems to require a disk mass of at least 0.04 M⊙ to operate (Boss, 2010).”
BackgroundInfluentialSelf-citationBoley, A. C., Payne, M. J., & Ford, E. B. (2012) · The Astrophysical Journal · doi:10.1088/0004-637x/754/1/57 · Cited by 69
“It is also possible that formation at moderate periods is not the only mode of planet formation, with at least some wide-orbit planets forming in situ by disk instability during the earliest stages of disk evolution (Boss 1997; Boley 2009).”
BackgroundSpezzi, L., de Marchi, G., Panagia, N., Sicilia-Aguilar, A., & Ercolano, B. (2011) · doi:10.1111/j.1365-2966.2011.20130.x · Cited by 37
“There is an ongoing debate about whether GI makes very massive disks fragment (Boss 1997, 2003; Cai et al. 2006, 2009), or simply favor accretion and mass transport (Hartmann et al. 2006).”
BackgroundDeep infrared imaging of close companions to austral A- and F-type stars
Ehrenreich, D., Lagrange, A. ‐., Montagnier, G., Chauvin, G., Galland, F., Beuzit, J.-L., & Rameau, J. (2010) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201014763 · Cited by 41
“The core-accretion theory (Pollack et al. 1996) is currently prefered to the gravitational instability theory (Boss 1997) as the origin mechanism of most planets detected by velocimetry because the latter mechanism is not expected to produce giant planets at distances <∼ 10 au (Rafikov 2005).”
BackgroundResolved images of self-gravitating circumstellar discs with ALMA
Cossins, P., Lodato, G., & Testi, L. (2010) · Monthly Notices of the Royal Astronomical Society · doi:10.1111/j.1365-2966.2010.16934.x · Cited by 37
“At radii greater than approximately 50AU, planet formation through direct fragmentation of these spiral overdensities into bound objects is possible (Boss 1997, 1998; Clarke 2009; Rafikov 2009; Cossins et al. 2010).”
BackgroundAstrometric signatures of giant-planet formation
Boss, A. (1998) · Nature · doi:10.1038/30177 · Cited by 37
Self-citationGravitational instability in a planet-forming disk
Speedie, J., Dong, R.-B., Hall, C., Longarini, C., Veronesi, B., Paneque-Carreño, T., Lodato, G., Tang, Y.-W., Teague, R., & Hashimoto, J. (2024) · Nature · doi:10.1038/s41586-024-07877-0 · Cited by 36
“1 and 2).”
Leconte, J., Baraffe, I., Chabrier, G., Barman, T., & Levrard, B. (2009) · Astronomy and Astrophysics · doi:10.1051/0004-6361/200911896 · Cited by 42
“The alternative so-called gravitational instability scenario for planet formation (Boss 1997) has been shown to be excluded, both on theoretical (Rafikov 2005, 2007) and numerical (Boley et al. 2007, see Dullemond et al. 2009 for a recent review) grounds, at least for planets within about 50 to 100…”
BackgroundThe Centurion 18 telescope of the Wise Observatory
Brosch, N., Polishook, D., Shporer, A., Kaspi, S., Berwald, A., & Manulis, I. (2008) · Astrophysics and Space Science · doi:10.1007/s10509-008-9752-4 · Cited by 36
“This, in turn, can be used to test predictions of planetary formation and evolution theories (Pollack et al. 1996, Boss 1997).”
BackgroundOrbital migration and the frequency of giant planet formation
Trilling, D. E., Lunine, J. I., & Benz, W. (2002) · Astronomy and Astrophysics · doi:10.1051/0004-6361:20021108 · Cited by 93
New chemical scheme for giant planet thermochemistry
Venot, O., Cavali'e, T., Bounaceur, R., Tremblin, P., Brouillard, L., & Brahim, R. L. B. (2020) · Astronomy & Astrophysics · doi:10.1051/0004-6361/201936697 · Cited by 35
“The knowledge of the deep composition of Solar System Giant Planets is essential to constrain their formation models (Pollack et al. 1996; Boss 1997; Owen et al. 1999; Gautier & Hersant 2005).”
BackgroundIdentifying and analysing protostellar disc fragments in smoothed particle hydrodynamics simulations
Hall, C., Forgan, D. H., & Rice, K. (2017) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stx1244 · Cited by 47
“…that metallicity variation makes very little difference to the occurrence of fragmentation (Boss 2002). c© 2016 The Authors In the GI scenario, gas giant planets and brown dwarfs form by direct gravitational collapse in the gaseous protostellar disc (Kuiper 1951; Cameron 1978; Boss 1997, 1998).”
BackgroundPLANETARY SYSTEM FORMATION IN THE PROTOPLANETARY DISK AROUND HL TAURI
Akiyama, E., Hasegawa, Y., Hayashi, M., & Iguchi, S. (2016) · The Astrophysical Journal · doi:10.3847/0004-637x/818/2/158 · Cited by 45
“In the GI, contrastingly, planets form in gravitationally unstable disks as stars form in gravitationally unstable molecular clouds (e.g., Boss 1997; Gammie 2001; Rafikov 2005; Cai et al. 2006; Kratter et al. 2010; Meru & Bate 2010).”
Background
Metadata
- Authors
- Boss, A. P.
- Affiliations
- Carnegie Institution for Science (US)
- Corresponding author
- Boss, Alan P.
- ORCID
- Boss, Alan P.
- Venue
- Science
- Published
- 1997-06-20
- Volume
- 276
- Issue
- 5320
- Pages
- 1836-1839
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2084110269
- Cited by
- 1,124
- References
- 0
- Citations by year
- 2026: 44 · 2025: 61 · 2024: 79 · 2023: 49 · 2022: 51 · 2021: 59 · 2020: 63 · 2019: 41 · 2018: 36 · 2017: 39 · 2016: 60 · 2015: 37 · 2014: 40 · 2013: 44 · 2012: 40
- FWCI
- 13.33
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Science (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astrophysics and Star Formation Studies
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Stellar, planetary, and galactic studies
- Keywords
- giant planet formation, gravitational instability, core accretion, protoplanetary disks, exoplanets, Jupiter, Saturn, isothermal disk, three-dimensional fluid dynamics, ice cores
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