Forward map from hillslope geometry (L, β, H; #29) and POLARIS soil properties (K, f; #30) to recession timescale and exponent priors, via hillslope Boussinesq theory:
- advection τ ≈
L·f / (K·sinβ)
- diffusion τ ≈
L²·f / (K·H) (same D = KH/f as the matrix-identifiability work)
- power-law exponent
b from the nonlinear Boussinesq solution
Complements the inverse Brutsaert–Nieber recession analysis with a geometry-based forward prior. Foundation for v4.0 field-data priors.
Depends on #29 + #30. Context: the recession-from-hillslope-geometry notes.
🤖 Generated with Claude Code
Forward map from hillslope geometry (
L,β,H; #29) and POLARIS soil properties (K,f; #30) to recession timescale and exponent priors, via hillslope Boussinesq theory:L·f / (K·sinβ)L²·f / (K·H)(sameD = KH/fas the matrix-identifiability work)bfrom the nonlinear Boussinesq solutionComplements the inverse Brutsaert–Nieber recession analysis with a geometry-based forward prior. Foundation for v4.0 field-data priors.
Depends on #29 + #30. Context: the
recession-from-hillslope-geometrynotes.🤖 Generated with Claude Code