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Interception Loss Calculator

Interception Loss Formula:

\[ I_i = S_i + (K_i \times E_r \times t) \]

mm
m/s
hours

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1. What is Interception Loss?

Interception Loss is the portion of the precipitation that is returned to the atmosphere through evaporation from plant surfaces or is absorbed by the plant. It represents the amount of rainfall that doesn't reach the ground surface due to vegetation cover.

2. How Does the Calculator Work?

The calculator uses the Interception Loss equation:

\[ I_i = S_i + (K_i \times E_r \times t) \]

Where:

Explanation: The equation calculates the total water loss through interception by considering the initial storage capacity of vegetation and the ongoing evaporation during rainfall.

3. Importance of Interception Loss Calculation

Details: Accurate interception loss calculation is crucial for hydrological modeling, water balance studies, and understanding how vegetation affects rainfall distribution and runoff generation.

4. Using the Calculator

Tips: Enter all values in the specified units. Interception Storage and Ratio values should be positive numbers. Evaporation Rate should be in m/s, and Duration in hours.

5. Frequently Asked Questions (FAQ)

Q1: What factors affect interception loss?
A: Vegetation type, density, rainfall intensity, duration, and meteorological conditions all influence interception loss.

Q2: How does vegetation type affect interception?
A: Different vegetation types have varying storage capacities and surface areas, leading to different interception rates.

Q3: Why convert time to seconds in the calculation?
A: Since evaporation rate is in m/s, time must be in seconds for unit consistency in the calculation.

Q4: What is typical range for interception storage?
A: Interception storage typically ranges from 0.5-2.0 mm for most vegetation types, depending on canopy characteristics.

Q5: How does interception affect water resources?
A: Interception reduces the amount of precipitation reaching the ground, affecting soil moisture, groundwater recharge, and surface runoff.

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