NOTES · DIMENSIONLESS
A sketching instrument, not a calibrated hydrodynamic model — values are abstract, not meters or hours.
  • Bed elevations: channel ≈ 40, marsh ≈ 130 (lower = deeper)
  • Flow: pixels per frame (~5 peak in the channel)
  • Tide: one cycle = 360 frames = one full flood + ebb
  • Asymmetry (M4): quarter-diurnal harmonic, 2× the tide frequency — drives net transport
  • Morphology: deposition/erosion, ramp saturates at ±60
TIDE
accretion +60   erosion −60
flow   sediment   spot elev. +12
drag dredge · shift+drag fill   |   sea ← inlet · land → right