If two 2-hour unit hydrograph are staggered by 2 hours and added graphically, the resulting hydrograph will be
4- hour unit hydrograph with 2 cm runoff
This question involves understanding the concept of a unit hydrograph (UH) and how hydrographs combine when a rainfall event is split into sequential parts.
A unit hydrograph is a hydrograph resulting from a direct runoff of a unit amount (typically 1 cm or 1 inch) of rainfall excess occurring uniformly over the drainage basin at a uniform rate for a specified duration.
In this scenario, we have a 2-hour unit hydrograph. This means it represents the basin's response to 2 hours of effective rainfall producing 1 cm of runoff.
When this 2-hour unit hydrograph is staggered by 2 hours, it implies that the rainfall event that generates this hydrograph is essentially treated as two consecutive 2-hour periods of rainfall excess, each producing 1 cm of runoff. The second pulse of rainfall excess starts 2 hours after the first.
Let's denote the first 2-hour unit hydrograph as UH1 and the second, staggered 2-hour unit hydrograph as UH2.
When these two hydrographs are added graphically, the resulting hydrograph's characteristics are determined as follows:
Time base = (Duration of UH) + (Staggering Interval)
Time base = $2 \text{ hours} + 2 \text{ hours} = 4 \text{ hours}$
Therefore, the resulting hydrograph represents the combined response to 2 cm of runoff, spread over a duration of 4 hours.
The combination of two 2-hour unit hydrographs, staggered by 2 hours, results in a hydrograph that reflects a total runoff depth of 2 cm and has a time base of 4 hours. This is described as a 4-hour unit hydrograph with 2 cm runoff, indicating the duration characteristics derived from the process and the total volume of runoff represented.
The use of unit hydrographs for estimating floods is generally limited to catchments of size less than?
What are the lower and upper limits of catchment area for applicability of the use of unit-hydrograph?
Select the correct option with regard to the following two statements (H1 and H2) pertaining to the hydrograph of a storm in a catchment.
H1: The rising limb of the hydrograph depends on the catchment characteristics only.
H2: The recession limb of the hydrograph depends on the storm characteristics and catchment characteristics.
Basin lag in hydrology is the time difference between the ______.
Isolated storm is represented in a hydrograph with