Title: Watershed Modeling Approaches
1Watershed Modeling Approaches
Distributed CASC-2D (CSU, U Conn, WMS)
- overland flow 2-D diffusion wave with explicit
FD - channel flow 1-D diffusion wave with explicit
FD, or 1-D dynamic wave with implicit Preissmann
scheme - infiltration Green-Ampt equation with
redistribution - evapotranspiration, interception, erosion
(overland and channel)
2Watershed Modeling Approaches CASC-2D
3Watershed Modeling Approaches CASC-2D
4Watershed Modeling Approaches
Soil Moisture Routing Model (Cornell)
- subsurface 2-D Darcys Law / water balance,
topography driven - evapotranspiration
- deep percolation
5Watershed Modeling Approaches
DHSVM
- Grid-based subsurface routing, hydraulic
gradient ground slope - Power law subsurface hydraulic conductivity
(transmissivity) function - Unit hydrograph distribution of excess runoff
(travel time for each pixel) - Muskingum-Cunge network/channel routing
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7Watershed Modeling Approaches
KINEROS2 (USDA-ARS)
- overland flow 1-D kinematic wave, 4-pt
implicit FD wetted area factor in recession - channel flow 1-D kinematic wave, 4-pt
implicit FD - infiltration Smith-Parlange, layered soils,
redistribution, interactive (plane to plane),
sub-grid effective parameters - erosion and sedimentation 4-pt implicit FD
- interception
8Watershed Modeling Approaches KINEROS2
9Watershed Modeling Approaches KINEROS2
10Watershed Modeling Approaches KINEROS2
11Watershed Modeling Approaches
TOPMODEL
- Topographically Driven slope, contributing
area, convergence - Saturated zone hydraulic gradient assumed to be
equal to slope - Exponential decrease of hydraulic conductivity
with depth - Watershed outflow related to mean depth to
water table - Saturation and infiltration excess runoff
generation - Evapotranspiration
- Channel routing kinematic wave
K0 surface conductivity, f decay coef., b
ground slope
12Watershed Modeling Approaches Topmodel
13Watershed Modeling Approaches
SAC-SMA (part of NWSRFS)
- Physically-based conceptual model
- based on physical concepts that describe water
movement trough a watershed - Lumped
- Continuous
- Two-layer soil model (upper and lower zones)
14Watershed Modeling Approaches SAC-SMA
Components
- Tension water (unsaturated)
- Free water (saturated)
- Surface flow
- Lateral drainage
- Evapotranspiration
- Vertical drainage (percolation)
15Watershed Modeling Approaches SAC-SMA
16Watershed Modeling Approaches SAC-SMA
17Watershed Modeling Approaches
- SAC-SMA is a component of NWSRFS
- Snow models available
- Runoff over a time step distributed to
watershed outlet using UH - Channel routing lumped methods, distributed
methods