Multi-wavelength study of the pre-eruption dip in the recurrent nova T Coronae Borealis preceding imminent nova eruption
Songpeng Pei, Xiaowan Zhang, Renzhi Su, Yongzhi Cai, Ziwei Ou, Qiang Li, Xiaoqin Ren, Taozhi Yang, Mingyue Li
TL;DR
The paper addresses how accretion-driven variability in the symbiotic recurrent nova T CrB manifests in a long, multi-wavelength dataset spanning quiescence, a prolonged high state, and the 2023–2025 pre-eruption dip. By integrating Swift XRT/BAT/UVOT with AAVSO photometry, the authors show a robust anti-correlation between X-ray and optical/UV emission and identify a wavelength-dependent fading during the pre-eruption dip, accompanied by soft and hard X-ray brightening and a subsequent second dip. They interpret these findings within an accretion-variation framework, linking a transition of the boundary layer from optically thick to thin to reductions in the mass-transfer rate that precede a thermonuclear runaway, consistent with but more complex than the 1946 event. This work provides a comprehensive, modern pre-eruption view that strengthens the case for using multi-wavelength accretion signatures as indicators of imminent nova eruptions in symbiotic recurrent systems, and it establishes a valuable baseline for future monitoring during the next outburst.
Abstract
We present a multi-wavelength study of the symbiotic recurrent nova (RN) T Coronae Borealis (T CrB) using Swift Burst Alert Telescope (BAT) / X-Ray Telescope (XRT) / UltraViolet Optical Telescope (UVOT) and American Association of Variable Stars Observers (AAVSO) observations from 2005 to 2025. Our analysis spans quiescent, high, and pre-eruption dip states. We find that brightening amplitudes increase toward shorter wavelengths in both optical and UV bands, while the UV and X-ray fluxes are generally anti-correlated throughout all phases. During the 2023-2024 pre-eruption dip, soft and hard X-rays increased as optical and ultraviolet (UV) brightness declined, consistent with a transition from an optically thick to thin boundary layer driven by a reduction in the accretion rate. We also report, for the first time, a second, lower-amplitude dip occurring between September 2024 and February 2025 following the primary 2023-2024 pre-eruption dip. The observed variability supports an accretion-variation scenario as a unifying explanation for both the high and dip states, and may signal an imminent nova eruption.
