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Besides the rainfall data itself, the most sensitive set of input parameters in a runoff model are the rainfall loss parameters.
Rainfall loss by canopy interception and subsequent evaporation to the atmosphere can be a significant portion of water loss from forested ecosystems.
For the performance analysis and design of rainwater tanks, a simple spreadsheet based daily water balance model was developed using daily rainfall data, contributing roof area, rainfall loss factor, available storage volume, tank overflow and rainwater demand.
With the aim of developing a comprehensive Decision Support Tool for the performance analysis and design of rainwater tanks, a simple spreadsheet based daily water balance model is developed using daily rainfall data, contributing roof area, rainfall loss factor, available storage volume, tank overflow and irrigation water demand.
With the aim of developing a comprehensive decision support tool for the performance analysis and design of rainwater tanks, a simple spreadsheet based daily water balance model was developed using daily rainfall data, contributing roof area, rainfall loss factor, available storage volume, tank overflow and rainwater demand.
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The SCS (NRCS) Curve Number approach is commonly used to compute rainfall losses.
Another method available for computing rainfall losses in HEC-1 is the Green and Ampt approach.
To be able to implement the modeling concept for streamflow predictions, the rainfall losses, most likely associated with interception losses not covered under the potential evapotranspiration calculation, would have to be more thoroughly analyzed through rainfall interception measurements.
total gross irrigation, total net irrigation, total irrigation losses, total percolation losses, actual water use by crop, potential water use by crop, effective rainfall, total rain loss, moist deficit at harvest, actual irrigation requirement, and.
Irregular rainfall and loss of topsoil means that the land produces less than before.
Rainfall interception loss was dominated by post-event evaporation of intercepted water rather than by within-event evaporation.
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