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PreprintCC BY 4.0arXiv

Bridging magnetothermal winds and photoevaporation to model discs dispersal

Abstract

Protoplanetary disc dispersal is driven by two processes usually modelled separately: photoevaporative and magnetohydrodynamic (MHD) disc winds. Global simulations indicate that in the inner disc these are not distinct outflows but a single magnetothermal wind. We assemble a closed-form, two-phase model that respects it. A single-field-line wind, whose base is fixed by the irradiated temperature and penetration column, supplies the launch and feeds a secular evolution, with photoevaporation convolved on as a sink. The flux closure Bz∝Σq is self-limiting: for q≤1/2 depletion alone cannot demagnetise the disc, so dispersal requires independent flux loss, parameterised by the magnetic Reynolds number ℛm. Integrating the coupled system yields two regimes. Efficient flux loss (ℛm≲1) lets the magnetisation front recede by over an order of magnitude and opens a photoevaporative gap. Flux retention (ℛm≫1) drives the front outward, sustains accretion, and defers dispersal by ≈2.7~Myr. Deriving the base from stellar irradiation instead of prescribing it, we find that the cold-launch approximation is valid during the early stages of disc evolution: anchoring the base at plasma equipartition (βbase ∼ 1) confines irradiation's influence on the magnetic lever arm to the magnetothermal annulus, decoupling the peak accretion rate from the incident flux. Both regimes clear the disc inside-out, through either a photoevaporatively amplified cavity wall or an expanding magnetothermal front.

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BibTeX
@misc{picogna2026bridging,
  title = {{Bridging magnetothermal winds and photoevaporation to model discs dispersal}},
  author = {Giovanni Picogna and Barbara Ercolano},
  howpublished = {arXiv},
  year = {2026},
  month = sep,
  doi = {10.48550/arxiv.2609.18334},
  eprint = {2609.18334},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2609.18334},
  note = {CC BY 4.0},
}
RIS
TY  - UNPB
TI  - Bridging magnetothermal winds and photoevaporation to model discs dispersal
AU  - Giovanni Picogna
AU  - Barbara Ercolano
PY  - 2026
DA  - 2026/09/18
PB  - arXiv
DO  - 10.48550/arxiv.2609.18334
UR  - https://arxiv.org/abs/2609.18334
AB  - Protoplanetary disc dispersal is driven by two processes usually modelled separately: photoevaporative and magnetohydrodynamic (MHD) disc winds. Global simulations indicate that in the inner disc these are not distinct outflows but a single magnetothermal wind. We assemble a closed-form, two-phase model that respects it. A single-field-line wind, whose base is fixed by the irradiated temperature and penetration column, supplies the launch and feeds a secular evolution, with photoevaporation convolved on as a sink. The flux closure B_z∝Σ^q is self-limiting: for q≤1/2 depletion alone cannot demagnetise the disc, so dispersal requires independent flux loss, parameterised by the magnetic Reynolds number ℛ_m. Integrating the coupled system yields two regimes. Efficient flux loss (ℛ_m≲1) lets the magnetisation front recede by over an order of magnitude and opens a photoevaporative gap. Flux retention (ℛ_m≫1) drives the front outward, sustains accretion, and defers dispersal by ≈2.7~Myr. Deriving the base from stellar irradiation instead of prescribing it, we find that the cold-launch approximation is valid during the early stages of disc evolution: anchoring the base at plasma equipartition (β_base ∼ 1) confines irradiation's influence on the magnetic lever arm to the magnetothermal annulus, decoupling the peak accretion rate from the incident flux. Both regimes clear the disc inside-out, through either a photoevaporatively amplified cavity wall or an expanding magnetothermal front.
ER  -