Gradient Formula:
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Waters Gradient refers to the slope or steepness of a watercourse, calculated as the change in elevation divided by the horizontal distance. It is a fundamental parameter in hydrology and geomorphology for understanding water flow characteristics.
The calculator uses the gradient formula:
Where:
Explanation: The formula calculates the rate of elevation change over a given horizontal distance, providing insight into the steepness of a watershed or river channel.
Details: Waters gradient is crucial for understanding stream velocity, sediment transport capacity, flood risk assessment, and watershed management. Steeper gradients typically indicate faster water flow and greater erosive power.
Tips: Enter the elevation change in meters and the horizontal distance in kilometers. Both values must be positive numbers greater than zero for accurate calculation.
Q1: What is a typical gradient range for rivers?
A: River gradients typically range from 0.1 m/km for lowland rivers to over 100 m/km for steep mountain streams.
Q2: How does gradient affect water flow?
A: Steeper gradients result in faster flow velocities, increased erosive power, and potentially higher flood risks during heavy rainfall events.
Q3: What units should I use for input?
A: Use meters for elevation change and kilometers for horizontal distance to get gradient in standard m/km units.
Q4: Can I use this for small streams?
A: Yes, the calculator works for any watercourse regardless of size, from small tributaries to major rivers.
Q5: How accurate is gradient calculation?
A: Accuracy depends on the precision of your elevation and distance measurements. Digital elevation models (DEMs) provide reliable data for gradient calculations.