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SWWRP Template PR

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Hydrologic Modeling System HEC-HMS Bill Scharffenberg U.S. Army Corps of Engineers Hydrologic Engineering Center HEC-HMS Background HEC-HMS is a complete engineering ... – PowerPoint PPT presentation

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Title: SWWRP Template PR


1
Hydrologic Modeling SystemHEC-HMS
Bill Scharffenberg U.S. Army Corps of
Engineers Hydrologic Engineering Center
2
HEC-HMS Background
  • HEC-HMS is a complete engineering hydrology
    simulation system with model components for
    meteorology, subbasins, river reaches,
    reservoirs, and diversion structures.
  • The subbasin component includes loss rate,
    surface transform, and baseflow subcomponents.
    Several model choices are available for each
    process.
  • The reach component includes several routing
    methods from simple empirical methods to
    sophisticated approximations of the dynamic wave
    equation.
  • The reservoir component can represent a dam using
    individual spillways, outlets, and other
    structures.

3
HEC-HMS Background
4
Gridded Simulation
  • Represent each subbasin as a collection of grid
    cells.
  • Gridded precipitation can come from radar
    rainfall, interpolated gage data, or atmospheric
    models.
  • For continuous simulation, gridded
    Priestley-Taylor evapotranspiration and gridded
    snowmelt.
  • Partially gridded loss methods use the same
    parameters and initial conditions but different
    boundary conditions for all grid cells in a
    subbasin.
  • Fully gridded loss methods use different
    parameters, initial conditions, and boundary
    conditions for each grid cell.

5
Gridded Simulation
6
Diversion Methods
  • The existing diversion element is limited to a
    user-supplied function of inflow.
  • Two new methods.
  • Lateral weir method uses a broad-crested spillway
    equation.
  • Pump station method uses a head-discharge pump.
  • Stage in the channel is computed from flow with a
    user-supplied stage-discharge curve.
  • Tailwater reductions are calculated with a second
    user-supplied stage-discharge curve representing
    flow characteristics on the "dry" side of the
    channel bank.
  • An optimization routine is used to compute the
    diversion flow for each time step, assuming the
    diversion is a point in the channel and there are
    no storage changes.

7
Diversion Methods
8
Spillway Gates
  • Reservoir element currently includes two
    spillways options without capability for gates
  • Broad-crested spillway
  • Ogee spillway
  • Add option for radial or vertical gates on both
    spillway types.
  • Each spillway can have up to 10 gate controls.
  • Each gate control can have different parameters
    and includes the number of identically operating
    gates.
  • Initially the only option for controlling the
    gates is a fixed opening height for the entire
    simulation enhancements are already planned for
    a future release.

9
Spillway Gates
10
Channel Losses
  • Percolation losses from the bottom of a streambed
    can be an important part of the water balance,
    especially in arid regions.
  • Constant loss method with equation
  • Percolation loss method.
  • Compute inundation area and multiply by
    percolation rate.
  • Revise all routing methods to include losses.
  • Use convergence algorithm to account for losses
    in the calculation of routed flow.

11
Channel Losses
12
Smith Parlange Loss Method
  • The Smith Parlange model approximates Richard's
    infiltration equation with the principal
    assumption
  • K approximation allows Richard's equation to be
    linearized while maintaining a reasonable
    functional relationship between K and water
    content T.
  • Significantly faster to solve than Richard's
    equation.
  • New research incorporated temperature affects.
  • Water density and viscosity.
  • Matric potential.

13
Smith Parlange Loss Method
14
Nonlinear Boussinesq Baseflow
  • Assumes an unconfined soil layer feeding
    baseflow.
  • Saturated at the end of a precipitation event.
  • Receives no recharge between events.
  • Requires Dupuit assumptions
  • Hydraulic gradient equal to the slope of the
    water table.
  • Streamlines are horizontal, equipotential lines
    are vertical.
  • Resulting equation
  • Parameters a and b in the equation can be
    computed using physical properties of the
    watershed.

15
Nonlinear Boussinesq Baseflow
16
Next Release
  • Targeted before end of 2006.
  • Development is 100 complete.
  • Testing is 90 complete.
  • Release decision expected soon.

www.hec.usace.army.mil/software/hec-hms/
17
Upcoming Development Work
  • Surface erosion subcomponent will be added to the
    subbasin.
  • Build-up and wash-off method.
  • Modified universal soil loss equation (MUSLE).
  • Nutrient subcomponent will be added to the
    subbasin element for simulating nitrogen and
    phosphorus processes.
  • New statistical summaries for continuous
    simulations will help support ecosystem studies.
  • New parameter estimation methods and tools will
    use optimization to better define parameters used
    in continuous simulation.
  • New methods for snowmelt and frozen ground
    simulation.
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