Formula Used:
From: | To: |
The formula calculates the area of catchment based on the peak discharge of a D-h unit hydrograph and the lag time of a 1-h unit hydrograph. It provides an estimation of the geographical area from which water flows into a particular point.
The calculator uses the formula:
Where:
Explanation: The formula accounts for the relationship between peak discharge, lag time, and catchment area in hydrological analysis.
Details: Accurate catchment area estimation is crucial for water resource management, flood prediction, and hydrological modeling. It helps in understanding water flow patterns and designing appropriate water management systems.
Tips: Enter peak discharge in m³/s and lag time in hours. All values must be valid positive numbers.
Q1: What is a unit hydrograph?
A: A unit hydrograph represents the direct runoff response of a catchment to a unit depth of excess rainfall over a specific duration.
Q2: How is lag time defined?
A: Lag time is the time interval from the midpoint of the rainfall excess to the peak discharge in the hydrograph.
Q3: What factors affect catchment area calculations?
A: Topography, soil type, land use, and rainfall characteristics can all influence catchment area calculations.
Q4: When is this formula most applicable?
A: This formula is particularly useful for hydrological modeling and flood prediction in medium to large catchments.
Q5: Are there limitations to this equation?
A: The formula may be less accurate for very small or very large catchments, or in areas with unusual hydrological characteristics.