We present a new model of giant planet formation that extends the core-accretion model of Pollack et al. (1996, Icarus, 124, 62) to include migration, disc evolution and gap formation. We show that taking these effects into account can lead to much more rapid formation of giant planets, making it compatible with the typical disc lifetimes inferred from observations of young circumstellar discs. This speed up is due to the fact that migration prevents the severe depletion of the feeding zone as observed in in situ calculations. Hence, the growing planet is never isolated and it can reach cross-over mass on a much shorter timescale. To illustrate the range of planets that can form in our model, we describe a set of simulations in which we ...
Previous simulations of planet formation utilizing single bodies including pebble accretion and plan...
Context. In the last few years, the so-called “Nice model” has become increasingly significant for s...
The inferred dust masses from Class II protoplanetary disc observations are smaller or equal to the ...
We present a new model of giant planet formation that extends the core-accretion model of Pollack et...
We extend the core-accretion model of giant gaseous planets by Pollack et al. ([CITE]) to include mi...
Context. According to the sequential accretion model (or core-nucleated accretion model), giant plan...
We present models of giant planet migration in evolving protoplanetary disks. Our disks evolve subje...
Giant planets migrate though the protoplanetary disc as they grow their solid core and attract their...
I present the results of semi-analytic calculations of migrating planets in young, outbursting circu...
The formation of planets depends on the underlying protoplanetary disc structure, which in turn infl...
We present N-body simulations of planetary system formation in thermally-evolving, viscous disc mode...
Giant planets migrate though the protoplanetary disc as they grow their solid core and attract their...
We present models of giant planet formation, taking into account migration and disk viscous evolutio...
Abstract. We present models of giant planet formation, taking into account migration and disk viscou...
We present a statistical study of the post-formation migration of giant planets in a range of initia...
Previous simulations of planet formation utilizing single bodies including pebble accretion and plan...
Context. In the last few years, the so-called “Nice model” has become increasingly significant for s...
The inferred dust masses from Class II protoplanetary disc observations are smaller or equal to the ...
We present a new model of giant planet formation that extends the core-accretion model of Pollack et...
We extend the core-accretion model of giant gaseous planets by Pollack et al. ([CITE]) to include mi...
Context. According to the sequential accretion model (or core-nucleated accretion model), giant plan...
We present models of giant planet migration in evolving protoplanetary disks. Our disks evolve subje...
Giant planets migrate though the protoplanetary disc as they grow their solid core and attract their...
I present the results of semi-analytic calculations of migrating planets in young, outbursting circu...
The formation of planets depends on the underlying protoplanetary disc structure, which in turn infl...
We present N-body simulations of planetary system formation in thermally-evolving, viscous disc mode...
Giant planets migrate though the protoplanetary disc as they grow their solid core and attract their...
We present models of giant planet formation, taking into account migration and disk viscous evolutio...
Abstract. We present models of giant planet formation, taking into account migration and disk viscou...
We present a statistical study of the post-formation migration of giant planets in a range of initia...
Previous simulations of planet formation utilizing single bodies including pebble accretion and plan...
Context. In the last few years, the so-called “Nice model” has become increasingly significant for s...
The inferred dust masses from Class II protoplanetary disc observations are smaller or equal to the ...