Landscape Processes

Input Rasters

All clipped to study area and coregistered

Name Description units
dem elevation m
precip precipitation 30 year norm m/day
T transmissivity of soil (Ksat * depth) m^2/day
$p_{s}$ particle bulk density of the soil kg/m^3
loss_factor ET and land use coeffictient (dimensionless)

Thresholds of landscape condition

Derived Rasters:

Input Description Source units
$a$ contributing area dem m^2
$b$ contour width dem pixel resolution m
$\theta$ slope dem degrees
$M$ slope: sine(theta) dem (dimensionless)
$q$ runoff precip * loss factor (ET, land use raster) m/day

Parameters:

Symbol Description Default Value units
$\tau$ critical sheer stress for channelization 16 Pa
$\phi$ internal friction angle 45 degrees
$k$ surface roughness 10000 (dimensionless)

Constants:

Symbol Description Value Units
$p_{w}$ water density 1000 kg/m^3
$g$ gravity constant 9.81 m/s^2
$v$ kinematic viscosity $1.31 * 10 ^(-6)$ m^2/s
seconds per day 86400 s/d

Saturated:

$\frac{a}{b}> \frac{T }{q}M$

Channelization:

$\frac{a}{b}> \frac{2\tau^3 }{p_{w}^{3}kvg^2M^2q} + \frac{T}{q}M$

Shallow Landsliding:

$\frac{a}{b}> \frac{p_{s}}{p_{w}} \left [ 1 - \frac{tan\theta}{tan\phi} \right ]\frac{T}{q}M$

Unconditionally stable:

$tan\theta < 0.5 tan\phi$

Unconditionally unstable

$tan\theta > tan\phi$

Landscape Condition Process Domain
Unsaturated Soil Creep
Saturated Sheet Wash
Channelized Channelization
Unconditionally Stable Landslide (wet)
Unconditionally Unstable Landslide (dry)