Differences

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--- start:hype_model_description:hype_np_soil [2019/12/19 16:20]
cpers [Soil erosion]
+++ start:hype_model_description:hype_np_soil [2019/12/19 16:44]
cpers [Soil erosion]
@@ Line 138: / Line 138: @@
 <m> MobilisedSR = {{(sflow*365)^{sreroexp}} * (1-common_{groundcover}) * {1/{0.5*soilcoh}} * sin(slope/100)} / 365 </m>
-All mobilized particles is not removed from the field, because sometimes the transport capacity of the particle-bearing water (//eflow//) will not suffice for the task. A //transportfactor// will reduce the particle amount:
+All mobilised particles is not removed from the field, because sometimes the transport capacity of the particle-bearing water (//eflow//) will not suffice for the task. A //transportfactor// will reduce the particle amount:
 <m> transportfactor = MIN(1.0,(eflow {/} 4)^{1.3}) </m>
-Eroded sediment (kg/km2) is calculated as:
+Mobilised sediment (kg/km2) is calculated as:
 <m> mobilSed = 1000 * (MobilisedRain + MobilisedSR) * transportfactor </m>
-The alternative erosion model calculates mobilized sediment (//mobilSed// (kg/km2)) based on rainfall (//rain//) and a number of model parameters and subbasin input data.
+The alternative erosion model calculates mobilised sediment (//mobilSed// (kg/km2)) based on rainfall (//rain//) and a number of model parameters and subbasin input data.
 <m> mobilSed = 1000. * ({slope / 5})^{erodslope} * erodluse * erodsoil * {EI/erodindex} * rain^{erodexp} </m>

HYPE Model Documentation