Through the main summer nectar flow, a strong colony is largely self-sufficient — foragers bring in nectar and pollen faster than beekeepers ever could by feeding, and the honey stores rise on their own. The two things a beekeeper can still usefully influence are water access and recognising when that flow suddenly stops. This lab puts a hive, a flower field and a water source side by side so you can watch forager traffic, honey stores and water stress respond to nectar flow, heat and where the water actually is.
The water stress index and the honey-store percentage are composite scores this simulation calculates from forager counts, temperature and water-source distance — useful, plausible stand-ins for colony condition, but model parameters rather than measurements from a real hive.
On a hot day a single strong colony can use several litres of water — placing even one shallow, pebble-filled dish near the hives is one of the few genuinely useful summer interventions a beekeeper can make, precisely because it doesn't interfere with foraging itself.
A hive, a flower field and a water source rendered side by side, so nectar flow, heat and how far water has to be carried each translate directly into forager traffic and rising or falling honey stores.
Nectar foragers (amber) and water foragers (cyan) split the workforce according to nectar flow and temperature, while fanning bees at the entrance scale up with heat to cool the hive — showing why water, not feeding, is the useful summer intervention.
Set active foragers, nectar flow and air temperature, then compare a nearby apiary dish against a distant natural source. Watch honey stores rise or fall and the water stress index respond in real time.
A single strong colony can use several litres of water on a hot day — placing one shallow, pebble-filled dish near the hives is one of the few genuinely useful summer interventions, precisely because it doesn't interfere with natural foraging.