A 12-hour storm occurs over a catchment and results in a direct runoff depth of 100 mm. The time-distribution of the rainfall intensity is shown in the figure (not to scale). The $\varphi$-index of the storm is (in mm, rounded off to two decimal places):

To calculate the $\varphi$-index, we use the following equation: \[ \varphi = \frac{\text{Total rainfall depth} - \text{Direct runoff depth}}{\text{Duration of the storm (in hours)}} \] From the given problem: - Total rainfall depth = 100 mm, - Direct runoff depth = 100 mm, - Duration of the storm = 12 hours. Now, we calculate the $\varphi$-index: \[ \varphi = \frac{100 \, \text{mm} - 100 \, \text{mm}}{12 \, \text{hours}} = 0.00 \, \text{mm/hour}. \] Thus, the $\varphi$-index of the storm is 0.00 mm.
A 12-hour storm occurs over a catchment and results in a direct runoff depth of 100 mm. The time-distribution of the rainfall intensity is shown in the figure (not to scale). The $\varphi$-index of the storm is (in mm, rounded off to two decimal places):

In Horton's equation fitted to the infiltration data for a soil, the initial infiltration capacity is 10 mm/h; final infiltration capacity is 5 mm/h; and the exponential decay constant is 0.5 /h. Assuming that the infiltration takes place at capacity rates, the total infiltration depth (in mm) from a uniform storm of duration 12 h is (round off to one decimal place)}
Consider a five-digit number PQRST that has distinct digits P, Q, R, S, and T, and satisfies the following conditions:
1. \( P<Q \)
2. \( S>P>T \)
3. \( R<T \)
If integers 1 through 5 are used to construct such a number, the value of P is:



