5.3 - Storm Hydrographs Flashcards
What is a storm hydrograph
A storm hydrograph is a graph showing variation in discharge (volume) of water at a given point over a short period of time, normally an individual storm ( few days)
What is the rising limb
The rising limb is the increase in river discharge, not necessarily instantaneously after precipitation
What is the peak discharge
The peak discharge is the maximum discharge, it occurs after a delay after maximum precipitation has occurred
What is lag time
Lag time is the time delay between peak discharge and precipitation
What is the falling limb
The falling limb shows the decline in discharge after peak flow as storm precipitation levels decrease
What is bankfull discharge
Bankfull discharge occurs when a rivers water levels reach the top of its channel. Any further increase will result in flooding of surrounding land
What is the normal ( base) flow
The normal base flow is the contribution to river flow from long term storage sources such as permeable rocks, areas of bog and marsh and peat covered moorlands
What would a flashy storm hydrograph look like
-a flashy storm hydrograph would have a short lag time , high peak discharge and steep rising limb
What would a subdued hydrograph look like
A subdued hydrograph would have a long lag time and low peak discharge
What size of drainage basin would be most likely to produce a flashy storm hydrograph and why
Small basins would be most likely to produce a flashy storm hydrograph as water will reach the channel rapidly as it has less distance to travel
What shape and relief type of drainage basin would be most likely to produce a flashy storm hydrograph
- A circular shaped basin would be most likely to produce a flashy hydrograph as it will take less time for water to reach the channel as all extremities are equidistant from the channel
- Steep sloped basins will produce a flashy storm hydrograph as water flows rapidly downhill and reaches the channel quickly
(Note - an elongated Basin will cause a subdued hydrograph as water will take a long time to reach the channel from the extremities of the basin)
What soil type will produce a flashy storm hydrograph
- clay soils and thin soils will cause a flashy storm hydrograph as clay should have a low porosity and the grains in the soil swell when they absorb water , so water infiltrates slowly.
- Thin soils also just become saturated quicksand
(note Sandy soils will produce a subdued hydrographas Sandy soils have high porosity so water can infiltrate effectively)
What type of land use will cause a flashy storm hydrograph
-Urban surfaces have more impermeable surfaces e,g roads so there is more run off, and there are more drains that carry water rapidly and directly to the river ( increasing discharge)
What type of evapotranspiration rates will cause a flashy storm hydrograph
Low evapotranspiration rates will cause a flashy storm hydrograph as low rates will mean that there are fewer losses from the drainage basin system and thus will cause an increase in discharge to the river channel
What type of drainage density will cause a flashy storm hydrograph
A large number of surface streams per km2 means more storm water will reach the main channel more quickly