The awakening of a classical nova from hibernation

TL;DR

This study presents long-term observations of nova V1213 Cen, providing evidence that nova eruptions can significantly increase the mass-transfer rate, supporting the hibernation model of cataclysmic variable star evolution.

Contribution

It offers the first direct observational evidence of a nova triggering a substantial increase in mass-transfer rate post-eruption, confirming a key aspect of the hibernation hypothesis.

Findings

Pre-eruption dwarf nova outbursts indicate low mass-transfer rate.

Post-eruption brightness increase by two orders of magnitude.

Absence of dwarf nova behavior after eruption suggests increased mass transfer.

Abstract

Cataclysmic variable stars (CVs) are close binary systems consisting of a white dwarf (primary) that is accreting matter from a low-mass companion star (secondary). From time to time such systems undergo large-amplitude brightenings. The most spectacular eruptions, over $10^4$ times in brightness, occur in classical novae and are caused by a thermonuclear runaway on the surface of the white dwarf. Such eruptions are thought to recur on timescales of $10^4-10^6$. In between, the system's properties depend primarily on the mass-transfer rate: if it is lower than a $10^{-9} M_{\odot}$/year, the accretion becomes unstable and the matter is dumped onto the white dwarf during quasi-periodic dwarf nova outbursts. The hibernation hypothesis predicts that nova eruptions strongly affect the mass-transfer rate, keeping it high for centuries after the event. Subsequently, the mass-transfer rate should significantly decrease for $10^3-10^6$ years, starting the hibernation phase. After that the nova awakes again - with accretion returning to the pre-eruption level and leading to a new nova explosion. The hibernation model predicts cyclical evolution of CVs through phases of high and low mass-transfer. The theory gained some support from the discovery of ancient nova shells around dwarf novae Z Cam and AT Cnc, but direct evidence for considerable mass-transfer changes prior, during and after nova eruptions has not hitherto been found. Here we report long-term observations of the classical nova V1213 Cen (Nova Cen 2009) covering its pre- and post-eruption phases. Within the six years before the explosion, the system revealed dwarf nova outbursts indicative of a low mass-transfer rate. The post-nova is two orders of magnitude brighter than the pre-nova at minimum light with no trace of dwarf nova behavior, implying that the mass-transfer rate increased considerably as a result of the nova explosion.