Height-dependent thermal properties of extreme-ultraviolet campfires in the quiet Sun
Small-scale impulsive energy-release events are widely considered a key ingredient of quiet-Sun coronal heating. We quantified the thermal-energy content of extreme ultraviolet (EUV) campfires, examined their impulsive heating characteristics, and investigated how their properties vary with atmospheric height. We analysed the complete campfire set from the 30 May 2020 Solar Orbiter/EUI observing sequence at 174 Angstrom, using SDO/AIA temperatures and emission measures, multiple volume models, cumulative distributions, and maximum-likelihood methods. We compared the results with Solar Orbiter/STIX microflares and SDO/AIA nanoflare-like events. Short-duration campfires occur at all heights, whereas longer-lived events preferentially occur in chromospheric layers. Emitting volumes and thermal energies show no comparable height dependence. Background-subtracted thermal energies span approximately $10^{20}$-$10^{24}$ erg, with rare events reaching $5\times10^{24}$ erg. The robust power-law regime extends over approximately $10^{22}$-$10^{24}$ erg; non-background-subtracted estimates are about one order of magnitude higher. Directly detected campfires contribute a sub-percent fraction of the canonical quiet-Sun heating requirement. Approximate corrections for the detection threshold and differential emission measure completeness could raise this to a few percent, but this remains a single-epoch, order-of-magnitude estimate. EUV campfires extend the flare energy distribution towards lower energies. The height dependence of durations, driven mainly by an excess of long-lived events in the lower chromosphere, alongside broadly invariant energy and volume distributions, indicates that atmospheric stratification primarily modulates cooling and dissipation timescales rather than the characteristic heating energy scale.