  On February 28, 2021, a fireball dropped $\sim0.6$ kg of recovered CM2
carbonaceous chondrite meteorites in South-West England near the town of
Winchcombe. We reconstruct the fireball's atmospheric trajectory, light curve,
fragmentation behaviour, and pre-atmospheric orbit from optical records
contributed by five networks. The progenitor meteoroid was three orders of
magnitude less massive ($\sim13$ kg) than any previously observed carbonaceous
fall. The Winchcombe meteorite survived entry because it was exposed to a very
low peak atmospheric dynamic pressure ($\sim0.6$ MPa) due to a fortuitous
combination of entry parameters, notably low velocity (13.9 km/s). A
near-catastrophic fragmentation at $\sim0.07$ MPa points to the body's
fragility. Low entry speeds which cause low peak dynamic pressures are likely
necessary conditions for a small carbonaceous meteoroid to survive atmospheric
entry, strongly constraining the radiant direction to the general antapex
direction. Orbital integrations show that the meteoroid was injected into the
near-Earth region $\sim0.08$ Myr ago and it never had a perihelion distance
smaller than $\sim0.7$ AU, while other CM2 meteorites with known orbits
approached the Sun closer ($\sim0.5$ AU) and were heated to at least 100 K
higher temperatures.
