Throw distance to arrival time, corrected for the air it travels through — temperature and humidity drive the math; altitude logs your local pressure.
Speed of sound uses the Bohn (1988) formula standard in AES live-sound literature:
c = 331.3 + 0.606×T + 0.0124×RH (T in °C, RH in %). Temperature dominates; humidity adds up to a few tenths of a m/s at typical stage conditions.
Barometric pressure has a negligible direct effect on the speed of sound in air — it cancels out in the ideal-gas relationship, a well-documented result in acoustic physics. Altitude here estimates your local station pressure via the International Standard Atmosphere model (P = P₀(1 − 0.0065h/288.15)^5.2559) purely so you can log real site conditions alongside a preset; it does not feed the timing math. Enter a live station reading to log the true value instead of the ISA estimate.
Arrival time is simply throw distance ÷ corrected speed of sound.
Sources: D. Bohn, “Environmental Effects on the Speed of Sound,” J. Audio Eng. Soc, 1988 · ICAO Standard Atmosphere, 1993.