For an annual flood series arranged in decreasing order of magnitude, the return period for a magnitude listed at position min a total of N entries is
This explanation details how to calculate the return period for an annual flood series, focusing on the correct formula based on the event's rank and the total number of entries.
An annual flood series is a list of flood events recorded over consecutive years. These events are typically arranged in decreasing order of magnitude. This means the largest flood recorded in the entire series is ranked first (position m=1), the second largest is ranked second (m=2), and so on, up to the Nth flood.
The return period (often denoted as T) represents the average time interval, usually in years, expected between occurrences of a flood event of a specific size or greater. For example, a 50-year return period flood is a flood magnitude that has, on average, a 1-in-50 chance of being equaled or exceeded in any given year.
To estimate the return period (T) for a specific flood event ranked 'm' in a series of 'N' total events, we use plotting position formulas. A widely accepted formula, particularly for annual series data, is the Weibull formula:
The formula is expressed as:
$$ T = \frac{N + 1}{m} $$
Where:
Let's compare the given options with the standard formula:
Based on standard hydrological practices for calculating the return period of flood events from an annual series ordered by magnitude, the correct formula uses the total number of entries (N) plus one, divided by the rank (m) of the event.
The relation between probability (P) and recurrence interval (T) is given by
The Muskingham’s method of flood routing through a river reach is primarily a
Muskingum method of routing satisfies the equation
For an annual flood series arranged in decreasing order of magnitude, the return period for a magnitude listed at position m’ in a total of N entries is
The formula for flood discharge are mostly of the form: