Earth
Sea and land breezes
Land warms and cools faster than water. Follow the circulation and switch between day and night.
The model and its limits
Two thermal reservoirs drive a damped circulation. The prescribed streamfunction conserves air volume; this is not CFD or a weather forecast. Height is exaggerated. 1 s = 20 min.
Equations used in the module
Equations C dT/dt = Q − λ(T − Tair); dU/dt = (0.7 ΔT − U)/900
