01 — The starting point
Why open air sounds different
Indoors, what reaches the audience is the sum of two things: what leaves the box directly and what bounces off walls, ceiling and floor. That second component does a lot of work for free. It fills the back of the room, gives a sense of body and lets a modest rig seem sufficient. Outdoors that gift does not exist: you only have direct sound, and direct sound follows one implacable rule.
Every time you double the distance from the box, the level drops by around 6 dB. If you have a comfortable level ten metres from the stage, at twenty metres you have lost half the sense of volume and at forty metres you are at a different event. Indoors that fall-off is much gentler because reverberation sustains the level at the back. Outdoors, the back gets nothing. That is why the classic mistake — two boxes at one end of the garden and hope — always produces the same outcome: the people at the front leave because it is too loud, and the people at the back cannot hear.
What you lose
The reflections, the envelopment and the containment of level. With no walls there is no free reinforcement, and nothing stops the sound travelling a mile and a half towards the neighbour's house.
What you gain
Intelligibility. With no reverberation, speech is far clearer than in an enclosed stone courtyard, and the risk of feedback with open microphones drops noticeably.
Add three phenomena that never show up inside. The first is air absorption: humidity and distance eat the high frequencies, so at thirty or forty metres the sound arrives dull even when it has level. You compensate with a touch of extra brightness in the distant boxes, not by pushing the master. The second is wind, which does more than put rumble in microphones: because it blows faster at height than at ground level, it bends the wavefront. Downwind the sound carries further than planned; upwind it lifts above the audience's heads and disappears.
The third causes the most trouble and almost nobody accounts for it: the night-time thermal inversion. By day the ground is warm and the air above it cooler, and sound tends to bend upwards. In the small hours the opposite happens — the ground cools faster than the air — and sound refracts downwards, skips off the terrain and travels much further. That is the physical reason why the level that disturbed nobody at ten in the evening can be heard across a whole village at two in the morning.
Mallorca tip
The ground matters more than people think. A sandstone courtyard or a compacted albero forecourt reflects and helps; a garden with long grass or an olive grove on loose soil absorbs an enormous amount, particularly in the midrange where the voice lives. The same configuration that is more than enough on a paved threshing floor falls short in a grove in the Pla. When we do a site visit, the ground surface is noted down alongside the available power.
Each type of space on the island behaves in its own way: we break it down venue by venue in the guide to event venues in Mallorca.