Viscous Gravity Current — Dam Break & Shallow Water Flow

Ritter (1892) exact dam-break solution vs. viscous gravity current spreading ~ t^(4/5)

Dam Break (Inviscid)

Viscous Current

Theory

Ritter dam-break (inviscid):
xfront = x₀ + 2√(gH₀)·t
h(x,t) = (1/9g)(2√(gH₀) − (x−x₀)/t)²
Valid: x₀−√(gH₀)t ≤ x ≤ x₀+2√(gH₀)t

Viscous current (Huppert 1982):
xN(t) ~ (g'V₀³/ν)^(1/5) t^(4/5)
h(x) ~ (xN−x) parabolic nose