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Question

The rate of rain fall for successive 30 minute periods of a 4 hour storm are 3.5, 4.5, 5.6, 8.5, 7.8, 6.4, 4.0, 3.8. taking ɸ- index as 5.0 compute W – index in cm/hr

The correct answer is

4.475

Calculating W-index from Rainfall Data and $\phi$-index

This problem involves calculating the W-index for a given storm using the provided rainfall rates and the $\phi$-index. The W-index is a measure of the overall infiltration rate during a storm event.

Here's the given information:

  • Duration of storm: 4 hours
  • Duration of each rainfall period: 30 minutes (0.5 hours)
  • Rainfall rates (cm/hr) for successive 30-minute periods: 3.5, 4.5, 5.6, 8.5, 7.8, 6.4, 4.0, 3.8
  • $\phi$-index: 5.0 cm/hr

The $\phi$-index represents the average rate of infiltration and other losses (like interception and depression storage) such that the volume of rainfall at intensities greater than the $\phi$-index equals the volume of direct runoff.

To calculate the W-index, we first need to determine the total rainfall and the total runoff based on the given $\phi$-index.

Step 1: Calculate Total Rainfall Depth

The total rainfall depth is the sum of the rainfall depths from each 30-minute period. Rainfall depth for a period is the rate multiplied by the duration (0.5 hours).

Let $R_i$ be the rainfall rate for period $i$, and $\Delta t = 0.5$ hr be the duration of each period.

Total Rainfall Depth $= \sum (R_i \times \Delta t)$

Total Rainfall Depth $= (3.5 \times 0.5) + (4.5 \times 0.5) + (5.6 \times 0.5) + (8.5 \times 0.5) + (7.8 \times 0.5) + (6.4 \times 0.5) + (4.0 \times 0.5) + (3.8 \times 0.5)$

Total Rainfall Depth $= 0.5 \times (3.5 + 4.5 + 5.6 + 8.5 + 7.8 + 6.4 + 4.0 + 3.8)$

Total Rainfall Depth $= 0.5 \times 44.1$

Total Rainfall Depth $= 22.05$ cm

Step 2: Identify Runoff-Producing Rainfall and Calculate Runoff Depth

Runoff occurs only when the rainfall intensity exceeds the $\phi$-index. The excess rainfall intensity ($R_i - \phi$) contributes to runoff during those periods.

Given $\phi$-index = 5.0 cm/hr.

Let's check which rainfall rates are greater than 5.0 cm/hr:

  • 3.5 cm/hr < 5.0 cm/hr (No runoff from this period)
  • 4.5 cm/hr < 5.0 cm/hr (No runoff from this period)
  • 5.6 cm/hr > 5.0 cm/hr (Runoff from this period)
  • 8.5 cm/hr > 5.0 cm/hr (Runoff from this period)
  • 7.8 cm/hr > 5.0 cm/hr (Runoff from this period)
  • 6.4 cm/hr > 5.0 cm/hr (Runoff from this period)
  • 4.0 cm/hr < 5.0 cm/hr (No runoff from this period)
  • 3.8 cm/hr < 5.0 cm/hr (No runoff from this period)

The rainfall rates that contribute to runoff are 5.6, 8.5, 7.8, and 6.4 cm/hr.

The runoff depth for each of these periods is $(R_i - \phi) \times \Delta t$.

Total Runoff Depth $= ((5.6 - 5.0) \times 0.5) + ((8.5 - 5.0) \times 0.5) + ((7.8 - 5.0) \times 0.5) + ((6.4 - 5.0) \times 0.5)$

Total Runoff Depth $= (0.6 \times 0.5) + (3.5 \times 0.5) + (2.8 \times 0.5) + (1.4 \times 0.5)$

Total Runoff Depth $= 0.3 + 1.75 + 1.4 + 0.7$

Total Runoff Depth $= 4.15$ cm

Step 3: Calculate Total Losses

Total Losses (infiltration, etc.) can be calculated as the difference between the Total Rainfall Depth and the Total Runoff Depth.

Total Losses = Total Rainfall Depth - Total Runoff Depth

Total Losses $= 22.05$ cm $- 4.15$ cm

Total Losses $= 17.9$ cm

Step 4: Calculate W-index

The W-index is defined as the total infiltration (total losses) during the storm divided by the total duration of the storm.

Total storm duration = 4 hours.

W-index $= \frac{\text{Total Losses}}{\text{Total Duration}}$

W-index $= \frac{17.9 \text{ cm}}{4 \text{ hr}}$

W-index $= 4.475$ cm/hr

The calculated W-index is 4.475 cm/hr.

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Important Questions from Precipitation

  1. Which rain gauge is NOT able to gives a plot of a mass curve of rainfall?

  2. Penman's equation is based on:
  3. Mean precipitation over an area is best obtained from the grouped amounts by

  4. _______ is caused by natural rising of warmer lighter air in colder denser surroundings.

  5. The process by which precipitation is caught and held by foliage, twigs and branches of the trees, shrubs and other vegetation, and lost by evaporation, never reaching the surface of the ground is known as

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