SPHY Manual - All versions
  • 📚Readme
  • manual
    • SPHY manual 3.1
      • Introduction
      • Theory
        • Background
        • Modules
        • Reference and potential evaporation
        • Dynamic vegetation processes
        • Snow processes
        • Glacier processes
        • Soil water processes
        • Soil erosion processes
        • Routing
      • Applications
        • Irrigation management in lowland areas
        • Snow- and glacier-fed river basins
        • Flow forecasting
        • Soil erosion and sediment transport
      • Installation of SPHY
        • Installing SPHY as a stand-alone application
          • Miniconda
          • SPHY v3.1 source code
      • Build your own SPHY-model
        • Select projection extent and resolution
        • Clone map
        • DEM and Slope
        • Delineate catchment and create local drain direction map
        • Preparing stations map and sub-basin.map
        • Glacier table
        • Soil hydraulic properties
        • Other static input maps
        • Meteorological forcing map series
        • Open water evaporation
        • Dynamic vegetation module
        • Soil erosion model input
          • MMF
          • Soil erosion model calibration
          • Soil erosion model output
        • Sediment transport
      • Reporting and other utilities
        • Reporting
        • NetCDF
      • References
      • Copyright
      • Appendix 1: Input and Output
      • Appendix 2: Input and Output description
      • Appendix 3: Soil erosion model input
        • MUSLE
        • INCA
        • SHETRAN
        • DHVSM
        • HSFP
    • SPHY manual 3.0
      • Introduction
      • Theory
        • Background
        • Modules
        • Reference and potential evaporation
        • Dynamic vegetation processes
        • Snow processes
        • Glacier processes
        • Soil water processes
        • Soil erosion processes
        • Routing
      • Applications
        • Irrigation management in lowland areas
        • Snow- and glacier-fed river basins
        • Flow forecasting
      • Installation of SPHY
        • General
        • Installing SPHY as a stand-alone application
          • Miniconda
          • SPHY v3.1 source code
      • Build your own SPHY-model
        • Select projection extent and resolution
        • Clone map
        • DEM and Slope
        • Delineate catchment and create local drain direction map
        • Preparing stations map and sub-basin.map
        • Glacier fraction map
        • Soil hydraulic properties
        • Other static input maps
        • Meteorological forcing map series
        • Open water evaporation
        • Dynamic vegetation module
        • Soil erosion model input
          • MUSLE
          • MMF
          • INCA
          • SHETRAN
          • DHVSM
          • HSFP
          • Soil erosion model calibration
          • Soil erosion model output
        • Sediment transport
        • Applications
        • Reporting
        • NetCDF
      • References
      • Copyright
      • Appendix 1: Input and Output
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  2. SPHY manual 3.1
  3. Appendix 3: Soil erosion model input

HSFP

The HSFP soil erosion model requires the following land use specific model parameters (hspf_table):

Table 41: Hspf_table

Land Use Class
Ground Cover (CR)
Soil Scour Detachment (KGER)
No Erosion

-99

1

2

3

1

0.65

0.03

0

2

0.5

0.2

0

3

0.35

0.5

0

…

…

…

…

Ground cover is similar to all other soil erosion models, specified per land use class. The soil scour detachment coefficient (KGER) is a model parameter that is a soil erodibility parameter for detachment by runoff. The “no erosion” column (0 or 1) prevents erosion from happening, for instance for water and paved land use classes.

The P-factor map indicates the support practice factor, which indicates how conservation measures reduce soil erosion, which factor is often considered to be 1.

The rainfall detachment coefficient KRER is similar to the USLE K-factor. The Wischmeier et al. (1971) formulations are used (see section 2.8) when this is left empty. In that case, a sand, clay and organic matter map should be provided in the PEDOTRANSFER section of the config file (even when the pedotransferfunctions are not used (i.e. if PedotransferFLAG = 0). The rainfall detachment exponent JRER is an exponent in the detachment by raindrop impact formulation.

Similar model parameters exist for the washoff detachment, i.e. KSER and JSER, and for scour detachment, i.e. KGER and JRER. The soil scour detachment KGER should be left empty when the land use specific values are provided in hspf_table.

The fraction by which detached sediment storage decreases per time step is defined by AFFIX.

Table 42: Model parameters

Model Parameter
Model Variable
Unit
Range/Default

Ground cover

CR

-

0-1

Soil scour detachment

KGER

-

0.01-0.5

No erosion

0 or 1

Support practice factor

SMPF

-

0-1

Rainfall detachment coefficient

KRER

-

0.14-0.45

Rainfall detachment exponent

JRER

-

1.5-3

Washoff detachment coefficient

KSER

-

0.1-5

Washoff detachment exponent

JSER

-

1.5-2.5

Soil scour detachment coefficient

KGER

-

0.01-0.5

Soil scour detachment exponent

JGER

-

1-2

Fraction of sediment storage decrease

AFFIX

-

0.05

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