Formula Used:
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The Total Storm Precipitation formula calculates the total precipitation from a storm event by combining direct runoff with the product of Φ-Index and duration of rainfall excess. This equation is fundamental in hydrology for water balance calculations and flood prediction.
The calculator uses the formula:
Where:
Explanation: The formula accounts for both the direct runoff component and the infiltration component of storm precipitation, providing a complete picture of water distribution during a storm event.
Details: Accurate precipitation calculation is crucial for hydrological modeling, flood forecasting, water resource management, and infrastructure design. It helps in understanding watershed behavior and predicting potential flood risks.
Tips: Enter total direct runoff in centimeters, Φ-Index in cm/h, and duration of rainfall excess in hours. All values must be non-negative numbers.
Q1: What is Φ-Index?
A: Φ-Index is the constant infiltration capacity that would yield the actual total runoff for a given rainfall amount. It represents the average infiltration rate during a storm event.
Q2: How is duration of rainfall excess determined?
A: Duration of rainfall excess is the total time during which rainfall intensity exceeds the infiltration capacity, typically determined from rainfall hyetograph analysis.
Q3: What are typical values for these parameters?
A: Values vary by region and soil type. Direct runoff typically ranges from 0-50 cm, Φ-Index from 0.1-5 cm/h, and duration from 0.1-48 hours depending on storm characteristics.
Q4: Are there limitations to this formula?
A: The formula assumes constant infiltration rate (Φ-Index) and may not accurately represent complex storm patterns or varying soil moisture conditions.
Q5: How is this used in practical applications?
A: This calculation is used in flood prediction models, drainage system design, irrigation planning, and environmental impact assessments.