Formula Used:
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The Mean of Z Variates represents the average value of the Z series for 'x' variate of a random hydrologic cycle in Log-Pearson Type III Distribution. It is a fundamental parameter in hydrological frequency analysis.
The calculator uses the formula:
Where:
Explanation: This formula calculates the mean value of Z variates by adjusting the Z series for a specific recurrence interval using the frequency factor and standard deviation of the sample.
Details: Accurate calculation of mean Z variates is crucial for hydrological modeling, flood frequency analysis, and water resource management. It helps in understanding the statistical properties of hydrological data and predicting extreme events.
Tips: Enter the Z series value for the desired recurrence interval, the appropriate frequency factor (typically between 5-30), and the standard deviation of the Z variate sample. All values must be valid numerical inputs.
Q1: What is the range of Frequency Factor (K_z)?
A: The frequency factor typically varies between 5 to 30 depending on rainfall duration and is a function of recurrence interval (T) and the coefficient of skew (Cs).
Q2: How is the Z Series for Recurrence Interval determined?
A: The Z series for any recurrence interval is derived from statistical analysis of hydrological data following Log-Pearson Type III distribution.
Q3: What does the Standard Deviation of Z Variate Sample represent?
A: It represents the dispersion of Z variate values around the mean and follows a certain probability distribution of the hydrological model.
Q4: When is this calculation typically used?
A: This calculation is primarily used in hydrological engineering for flood frequency analysis, dam design, and water resource planning.
Q5: Are there limitations to this formula?
A: The accuracy depends on the quality of input data and the appropriateness of the Log-Pearson Type III distribution for the specific hydrological dataset.