Fog forms when air close to the ground cools to saturation and water vapour condenses into tiny droplets. Radiation and advection fog reach that point by different routes.
Lightning heats a long, crooked channel of air so quickly that it drives a pressure wave. Distance and channel shape turn that wave into a crack or rumble.
Jet exhaust starts a trail of ice crystals, but the surrounding upper air decides whether it vanishes, breaks into segments or spreads into cirrus cloud.
A heat dome is not a lid in the sky. It is a persistent high-pressure pattern that keeps air sinking and lets heat build. Here is why cooler nights matter.