pith:56SMOWRR
$\alpha\beta q_\mathrm{th}$-mapping of planet-induced density wave damping in protoplanetary discs
Nonlinear shocks usually dominate damping of planet-launched density waves, but cooling on orbital timescales rivals them for sub-thermal planets while viscosity needs high values to matter.
arxiv:2605.12607 v1 · 2026-05-12 · astro-ph.EP
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Claims
nonlinear wave evolution leading to shock formation is typically the most important cause of angular momentum deposition, but that cooling on timescales comparable to local orbital time reaches similar levels of importance for low mass planets (sub-thermal, q_th<1). On the contrary, linear wave damping due to viscosity is rather inefficient, requiring α ≳ 10^{-1.5} to noticeably affect damping of waves launched by thermal mass planets.
The hydrodynamic simulations capture all relevant damping physics without missing contributions from magnetic fields, realistic radiative transfer, or three-dimensional effects that could alter the relative importance of the three mechanisms.
Nonlinear shock formation dominates angular momentum deposition from planet-induced density waves, cooling matches it for sub-thermal planets, and viscosity only matters at unrealistically high values.
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| First computed | 2026-05-18T03:10:00.712964Z |
|---|---|
| Builder | pith-number-builder-2026-05-17-v1 |
| Signature | Pith Ed25519
(pith-v1-2026-05) · public key |
| Schema | pith-number/v1.0 |
Canonical hash
efa4c75a31a99b396a221b1f110c59706e1e094734d93c8d9c696a93e67aa606
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curl -sH 'Accept: application/ld+json' https://pith.science/pith/56SMOWRRVGNTS2RCDMPRCDCZOB \
| jq -c '.canonical_record' \
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Canonical record JSON
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