🌬️ Wind Erosion

Threshold u*t—
Transport Q—
Dune height—
Deflation depth—
Mode—
Bagnold Transport
u*t = A·√((ρp−ρa)·g·d / ρa)
Q = C·(u*³ − u*t³)

Saltation: grains bounce. Creep: surface grains roll. Dunes form via deposition feedback.