Gauge Height Formula:
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The Gauge Height formula calculates the height of water in a stream above a reference point based on discharge and rating curve parameters. It is particularly useful for non-alluvial rivers where the relationship between discharge and water level follows a predictable pattern.
The calculator uses the Gauge Height formula:
Where:
Explanation: The formula establishes a power-law relationship between discharge and water level, with constants specific to each river's rating curve.
Details: Accurate gauge height estimation is crucial for flood forecasting, water resource management, hydraulic engineering, and environmental monitoring in non-alluvial river systems.
Tips: Enter discharge in m³/s, rating curve constants, and gauge reading constant. All values must be valid positive numbers with appropriate precision.
Q1: What are typical values for rating curve constants?
A: Rating curve constants vary by river but typically range from 1.5-2.5 for Cr and 1.2-2.0 for β, depending on channel characteristics.
Q2: How is the constant 'a' determined?
A: Constant 'a' is determined through field measurements as the gauge reading when discharge is zero, representing the channel bottom elevation.
Q3: Why is this formula specific to non-alluvial rivers?
A: Non-alluvial rivers have stable channels with consistent rating curves, while alluvial rivers experience bed changes that alter the discharge-stage relationship.
Q4: How often should rating curves be updated?
A: For non-alluvial rivers, rating curves typically remain valid for several years but should be verified annually with current measurements.
Q5: What are the limitations of this formula?
A: The formula assumes a stable channel and may not accurately represent extreme flood conditions or situations with backwater effects.