WMS:OC Losses: Difference between revisions
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Watershed outflow in Orange County is a function of losses. Examples of losses include depression storage, vegetation interception and transpiration, minor amounts of evaporation, and infiltration. Many, if not all, of these losses are affected by the land cover or soil type. | Watershed outflow in Orange County is a function of losses. Examples of losses include depression storage, vegetation interception and transpiration, minor amounts of evaporation, and infiltration. Many, if not all, of these losses are affected by the land cover or soil type. | ||
Fm, or the maximum loss rate, is a measurement of the effect of these losses on the [[WMS:OC Rational Equation|peak flow rate]]. This value corresponds to the soil group, cover complex, and imperviousness of the drainage subarea. Fm is calculated by the following equation: <math>Fm = ap * Fp</math> where, | <math>Fm</math>, or the maximum loss rate, is a measurement of the effect of these losses on the [[WMS:OC Rational Equation|peak flow rate]]. This value corresponds to the soil group, cover complex, and imperviousness of the drainage subarea. <math>Fm</math> is calculated by the following equation: <math>Fm = ap * Fp</math> where, | ||
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Revision as of 21:26, 13 February 2013
Watershed outflow in Orange County is a function of losses. Examples of losses include depression storage, vegetation interception and transpiration, minor amounts of evaporation, and infiltration. Many, if not all, of these losses are affected by the land cover or soil type.
, or the maximum loss rate, is a measurement of the effect of these losses on the peak flow rate. This value corresponds to the soil group, cover complex, and imperviousness of the drainage subarea. is calculated by the following equation: where,
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