The Inter-Eruption Timescale of Classical Novae from Expansion of the Z Camelopardalis Shell
Michael M.Shara, Trisha Mizusawa, David Zurek, Christopher D. Martin,, James D. Neill, Mark Seibert

TL;DR
This study uses the expansion of the Z Camelopardalis shell to estimate the inter-eruption timescale of classical novae, providing the first strong observational test of the >1000-year recurrence prediction.
Contribution
It presents the first observational constraint on the inter-eruption timescale of classical novae using shell expansion measurements, supporting the theory that these intervals exceed 1000 years.
Findings
Lower limit of 1300 years for the last eruption of Z Cam
No detectable shell expansion over 3 years, with an upper limit of 1 pixel/3 years
Ejecta velocity estimated at 85 km/s if associated with the 77 BCE nova
Abstract
The dwarf nova Z Camelopardalis is surrounded by the largest known classical nova shell. This shell demonstrates that at least some dwarf novae must have undergone classical nova eruptions in the past, and that at least some classical novae become dwarf novae long after their nova thermonuclear outbursts. The current size of the shell, its known distance, and the largest observed nova ejection velocity set a lower limit to the time since Z Cam's last outburst of 220 years. The brightest part of the Z Cam shell's radius is currently p ~ 1690 pixels. No expansion of the radius of the brightest part of the ejecta was detected, with an upper limit of pdot < 1 pixel/3 years. This suggests that the last Z Cam eruption occurred p/pdot > 5,000 years ago. However, including the important effect of deceleration as the ejecta sweeps up interstellar matter in its snowplow phase reduces the lower…
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