Formula Used:
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Distance along Main Water Course from the gauging station to a point opposite to the watershed centroid is a key hydrological parameter used in watershed analysis and flood forecasting. It represents the flow path distance in the main water channel.
The calculator uses the formula:
Where:
Explanation: This formula calculates the distance along the main water course using basin characteristics including lag time, length, slope, and specific basin constants.
Details: Accurate calculation of distance along the main water course is crucial for hydrological modeling, flood routing, watershed management, and designing hydraulic structures.
Tips: Enter all required parameters with appropriate units. Ensure all values are positive and within reasonable ranges for accurate results.
Q1: What is Basin Lag?
A: Basin Lag is the elapsed time between the occurrences of the centroids of the effective rainfall and the resulting runoff hydrograph.
Q2: How is Basin Constant determined?
A: Basin Constant is typically derived from regional hydrological studies and varies based on watershed characteristics and geographical location.
Q3: Why is Basin Slope important in this calculation?
A: Basin Slope affects the flow velocity and travel time in the water course, making it a critical factor in distance calculations.
Q4: What are typical values for Basin Constant 'n'?
A: Basin Constant 'n' typically ranges between 0.3-0.8 depending on watershed characteristics and regional hydrological conditions.
Q5: How accurate is this calculation method?
A: The accuracy depends on the quality of input parameters and how well they represent the actual watershed conditions. Regional calibration may be needed for specific applications.