The disc instability model: original recipe and additional ingredients
Jean-Marie Hameury
TL;DR
The paper assesses the Disk Instability Model (DIM) and its extensions for cataclysmic variables, focusing on how additional ingredients—disc truncation, irradiation (hot-white-dwarf and self-irradiation), mass-transfer variations, stream overflow, and winds—alter stability and light-curve behavior. It discusses a 1D adaptive-grid implementation with a two-value $ ext{α}$ viscosity and an $S$-curve, showing that each ingredient shifts the stability boundaries and can reproduce diverse outburst morphologies, including long recurrence times and complex rebrightenings. However, the proliferation of poorly constrained parameters limits predictive power, and multiple mechanisms can explain similar phenomena (e.g., long outbursts via tidal instabilities or irradiation-driven mass transfer). The author argues for progress through intermediate 2D simulations that relax axisymmetry while leveraging accurate vertical structure, and for addressing outstanding issues such as low states, disc truncation physics, and the role of magnetic fields, to solidify the physical basis of the DIM.
Abstract
The disc instability model successfully reproduces many of the observed properties of cataclysmic variables. However, additional ingredients such as mass-transfer variations, disc irradiation, stream-disc overflow, or inner-disc truncation must be included to explain certain systems. The physics underlying these processes is often poorly constrained, and our lack of knowledge is typically absorbed into extra free parameters, much like the $α$-prescription for viscosity. In this paper, I examine how each of these ingredients affects the predicted light curves and discuss the limitations that arise from the growing number of unconstrained parameters on the model's predictive power.
