A Spreading Layer Origin for Dwarf Nova Oscillations

Abstract

Dwarf nova outbursts often show coherent (Q ~ 104-106) sinusoidal oscillations with the largest pulsed fraction in the extreme ultraviolet. Called dwarf nova oscillations (DNOs), they have periods of P ≈ 3-40 s and scale with luminosity as P ∝ L-β with β ≈ 0.1-0.2. We propose that DNOs may be produced by nonradial oscillations in a thin hydrostatic of freshly accreted material, the spreading layer (SL), at the white dwarf (WD) equator. This would naturally explain a number of key properties of DNOs, including their frequency range, sinusoidal nature, sensitivity to accretion rate, and why they are only seen during outburst. In support of this hypothesis, we construct a simple model that treats the SL as a cavity containing shallow surface waves, each with the same radial structure, but split into three different modes denoted by their azimuthal wavenumber, m. The m = 0 latitudinally propagating mode best matches the periods and scalings associated with most DNOs, and DNOs with periods shorter than the WD Keplerian period are explained by the m = -1 prograde mode. We also predict a third set of oscillations, produced by the m = 1 retrograde mode, and show its expected dependence on accretion rate.