factors affecting floods Flashcards
bifurcation ratio
how many L1 streams can create an L2 streams when they merge together
- lower ratio = water is only concentrated in one channel
rock types [geological factors]
permeability of rocks:
- more permeable rock = higher likelihood of infiltration taking place
- also represents amount of base/throughflow
- lower hydrograph peaks & higher lag time
land use
e.g. how vegetation cover increases lag time
- contributes to interception storage & higher infiltration rates]
- influences lag time & peak discharge
drainage density
how frequently streams occur on land
- average length of a stream within a unit area, influenced by climate & geology
- higher density = higher flood peaks [water flows faster in the channels]
relief
difference between the heights of high and low points on a map
- steeper slope = higher peaks & steeper rising limb in a hydrograph
basin circularity
more circular basin = higher peaks & lower lag time
- the distance that water has to cover to enter & exit the basin is the same all around due to similar radius
basin elongation [part of circularity]
largest dimension of basin with the circle’s diameter
- more elongated basin = lower peaks and higher lag time [water arrives in a staggered fashion]
precipitation type
heavier ppt = rapid overland flow generation
- infiltration rate is overwhelmed with too much ppt
- results in a flashy hydrograph