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Rainfall In Inches By Khosla's Formula Calculator

Khosla's Formula:

\[ RPI = RKI + \frac{(T_f - 32)}{9.5} \]

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°F

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1. What is Khosla's Formula?

Khosla's Formula is used to estimate rainfall depth in inches based on runoff depth and temperature. It provides a method to calculate rainfall intensity and distribution for hydrological studies and water resource management.

2. How Does the Calculator Work?

The calculator uses Khosla's Formula:

\[ RPI = RKI + \frac{(T_f - 32)}{9.5} \]

Where:

Explanation: The formula accounts for the relationship between runoff depth, temperature, and resulting rainfall depth, with temperature adjustment factor based on Fahrenheit scale.

3. Importance of Rainfall Depth Calculation

Details: Accurate rainfall depth estimation is crucial for hydrological modeling, flood prediction, irrigation planning, and water resource management in agricultural and urban environments.

4. Using the Calculator

Tips: Enter runoff depth in inches and temperature in Fahrenheit. Ensure valid values are provided (runoff depth ≥ 0).

5. Frequently Asked Questions (FAQ)

Q1: What is the practical application of Khosla's Formula?
A: Khosla's Formula is primarily used in hydrological studies to estimate rainfall patterns and intensity for watershed management and irrigation planning.

Q2: Why is temperature included in the rainfall calculation?
A: Temperature affects evaporation rates and water cycle dynamics, making it an important factor in rainfall-runoff relationships.

Q3: What are typical values for runoff depth?
A: Runoff depth values vary significantly based on soil type, land use, and precipitation intensity, typically ranging from 0 to several inches.

Q4: Are there limitations to this formula?
A: The formula provides an estimation and may not account for all local factors such as soil moisture, vegetation cover, or topography.

Q5: Can this formula be used for all climate conditions?
A: While generally applicable, the formula may require calibration for specific regional conditions and extreme climate scenarios.

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