Green’s function solutions reveal how magnetically driven winds affect accretion disk evolution over time.
We present Green’s function solutions for a geometrically thin, one-dimensional Keplerian accretion disk that includes angular momentum extraction and mass loss due to magnetohydrodynamic (MHD) winds. The disk viscosity is assumed to vary radially as ν∝rn. We derive solutions for three types of boundary conditions applied at the inner radius rin: (i) zero torque, (ii) zero mass accretion rate, and (iii) finite torque and finite accretion rate, and investigate the time evolution of a disk with an initial surface density represented by a Dirac-delta function. The mass accretion rate at the inner radius decays with time as t−3/2 for n = 1 at late times in the absence of winds under the zero-torque condition, consistent with Lynden-Bell & Pringle (1974), while the presence of winds leads to a steeper decay. All boundary conditions yield identical asymptotic time evolution for the accretion and wind mass-loss rates, though their radial profiles differ near rin. Applying our solutions to protoplanetary disks, we find that the disk follows distinct evolutionary tracks in the accretion rate-disk mass plane depending on ψ, a dimensionless parameter that regulates the strength of the vertical stress driving the wind, with the disk lifetime decreasing as ψ increases due to enhanced wind-driven mass loss. The inner boundary condition influences the evolution for ψ < 1 but becomes negligible at higher ψ, indicating that strong magnetically driven winds dominate and limit mass inflow near the boundary. Our Green’s function solutions offer a general framework to study the long-term evolution of accretion disks with magnetically driven winds.
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T. Mageshwaran (2026) studied this question.
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