Formula Used:
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The First Moment of the ERH (Effective Rainfall Hydrograph) about the time origin divided by the total effective rainfall is a key parameter in hydrological analysis. It represents the temporal distribution characteristics of effective rainfall in a catchment area.
The calculator uses the formula:
Where:
Explanation: This formula calculates the first moment of the effective rainfall hydrograph by subtracting the product of constants n and K from the first moment of the direct runoff hydrograph.
Details: Calculating the first moment of ERH is crucial for understanding the timing and distribution of effective rainfall in hydrological modeling, flood forecasting, and watershed management studies.
Tips: Enter the first moment of DRH (MQ₁), constant n, and constant K. All values must be non-negative numbers. The calculator will compute the first moment of ERH (MI₁).
Q1: What is the significance of the first moment in hydrology?
A: The first moment represents the centroid or average time of the hydrograph, providing important information about the timing characteristics of rainfall or runoff.
Q2: How are constants n and K determined for a catchment?
A: Constants n and K are typically determined through calibration using historical rainfall and runoff data specific to the catchment characteristics.
Q3: What units are used for the first moment calculation?
A: The first moment is typically expressed in time units (hours or minutes) as it represents the temporal distribution of the hydrograph.
Q4: Can this formula be applied to all catchment types?
A: While the formula is generally applicable, constants n and K need to be calibrated specifically for each catchment to ensure accurate results.
Q5: What is the relationship between ERH and DRH?
A: The Effective Rainfall Hydrograph (ERH) represents the rainfall excess that becomes direct runoff, while the Direct Runoff Hydrograph (DRH) represents the catchment's response to this effective rainfall.