3. Hydrographs Flashcards
What is a Hydrograph?
A hydrograph is a means of showing the discharge of a river at a given point over a short period of time (an individual rainfall event)
Cumecs
Cubic Metres per Second
Peak Flow / Peak Discharge
The highest level of water reached during a flood
Bankfull Discharge
When the river is completely full - if it rises further there will be flooding!
Rising Limb
Measures increasing discharge over time. Steeper limb = flashier flood!
Falling Limb / Recession
Measures discharge after peak discharge / heavy flow.
- Decreasing in steepness
- Less steep than rising limb because of throughflow now reaching river (to increase water level).
Runoff / Storm Flow
Stream discharge after a rainstorm, produced by a combination of overland flow and then throughflow (overland makes greatest contribution).
Base Flow
(Normal flow ) - stream discharge produced by water seeping from bedrock
Lag Time
The difference between peak rainfall and peak discharge.
Rainfall Peak
The maximum volume of rainfall that occurrs in a storm event.
Approach Segment
The discharge before rainfall
Infiltration Capacity
The maximum rate at which the soil will absorb water
Rainfall Intensity
Amount of rain in a given time
If infiltration capacity is greater than rainfall intensity…
…the stores (capacity of the soil to store water) will fill up before overland flow occurs. This is typical of many locations in the UK.
If infiltration capacity is lower than rainfall intensity…
…then rapid runoff occurs (known as Hortonian flow). Water cannot enter the ground so it runs straight off.
This often occurs in hot arid and seri-arid environments.