Evolution of the recent high-accretion state of the recurrent nova T CrB: HST, Swift, NuSTAR, and XMM-Newton observations
G. J. M. Luna, N. P. M. Kuin, K. Mukai, J. L. Sokoloski, K. Page, J. P. Osborne
TL;DR
This study presents a comprehensive, multiwavelength view of the recurrent nova T CrB as it enters a super-active state (SAS) and transitions to a faint state. By integrating HST, Swift, NuSTAR, XMM-Newton, and AAVSO optical data, it demonstrates that the SAS is driven by an increased mass accretion rate, causing the boundary layer to become optically thick and producing a soft X-ray (blackbody-like) component, while the optically thin cooling-flow emission rises as the system approaches eruption. The analysis finds no evidence for a ~6000 s periodic signal after accounting for red noise, argues against dust obscuration for the dip, and highlights intrinsic accretion-related variability as the dominant driver of the observed changes. A self-consistent framework links the SAS evolution to accretion-disk structure changes and boundary-layer dynamics, though precise eruption timing remains uncertain due to large scatter in recurrence intervals. The work provides a solid baseline for predicting pre-eruption behavior and informs models of mass accumulation in quiescent phases of recurrent novae.
Abstract
As the recurrent nova T Coronae Borealis (T CrB) approaches its next predicted thermonuclear eruption, it is currently exhibiting a "super-active state" (SAS) characterized by enhanced multiwavelength emission similar to the behavior recorded prior to the 1946 outburst. We present a multiwavelength analysis of the SAS and the subsequent "faint state" using observations from HST, Swift, NuSTAR, and XMM-Newton. Our results indicate that the SAS was driven by an increase in the mass accretion rate, which caused the accretion disk's boundary layer to become optically thick. A weighted least squares regression analysis quantifies the evolution of the accretion components, displaying a highly significant (4.5$σ$) increase in the luminosity of the optically thin cooling flow (L$_{cf}$) and a marginal (2.58$σ$) decrease in the optically thick boundary layer luminosity (L$_{bb}$) as the system transitioned into the faint state. We find that this dimming is consistent with an intrinsic change in the accretion flow rather than dust obscuration, supported by the lack of infrared excess and the stability of the 2175 Å feature. Additionally, a time-series analysis using autoregressive modeling to account for correlated red noise revealed no significant periodicities, thereby disputing the previously reported $\sim$6000 s signal. These findings suggest that the pre-outburst evolution of T CrB is characterized by significant changes in the accretion disk structure and boundary layer, providing a self-consistent physical framework for the system's behavior as it approaches eruption.
