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start:hype_model_description:hype_sediment

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start:hype_model_description:hype_sediment [2019/12/19 16:41]
cpers [Links to file reference]
start:hype_model_description:hype_sediment [2020/02/28 10:42] (current)
cpers [Soil erosion]
Line 37: Line 37:
 <m> mobilSed = 1000 * (MobilisedRain + MobilisedSR) * transportfactor </m> <m> mobilSed = 1000 * (MobilisedRain + MobilisedSR) * transportfactor </m>
    
-//Soil erosion model 2 (HBV-SED based model)//: The second model is based on HBV-SED model (Lidén, 1999; Lidén et al., 2001) and calculates particles mobilized by rain (//​rain//​). ​It also depends on soil and land characteristics in the form of model parameters and data on subbasin characteristics. ​+//Soil erosion model 2 (HBV-SED based model)//: The second model is based on HBV-SED model (Lidén, 1999; Lidén et al., 2001) and calculates particles mobilized by rain (//​rain//​). ​When the ground is frozen or there is snow on the ground, the no particles are mobilized. The mobilization ​also depends on soil and land characteristics in the form of model parameters and data on subbasin characteristics. ​
  
 <m> mobilSed = 1000. * ({slope / 5})^{erodslope} * erodluse * erodsoil * {EI/​erodindex} * rain^{erodexp} </m> <m> mobilSed = 1000. * ({slope / 5})^{erodslope} * erodluse * erodsoil * {EI/​erodindex} * rain^{erodexp} </m>
start/hype_model_description/hype_sediment.1576770110.txt.gz · Last modified: 2019/12/19 16:41 by cpers