Surface Water 2 - Overland Flow Flashcards
Overland Flow
- Non-Channeled water flow on ground surface
Factors that influence overland flow
- Precipitation intensity
- Snow melt rate (rapid or over months)
- Pre-existing soil saturation level (saturated will cause flow)
- Soil Type (hydraulic permeability
- Ground Cover
- Topography/Terrain characteristics (slopes vs. flats)
Types of surface runoff during rainfall or snowmelt
- Infiltration excess overland flow (Hortonian)
- Saturation excess overland flow
Hortonian overland flow
- Occurs when soil is not saturated
- Soil properties or land cover do not allow infiltration to keep up with rain/snow melt rates
- Rainfall rate > infiltration capacity = Overland flow
Saturation excess overland flow
- Occurs when soil becomes saturated and there is no longer any space for water to infiltrate
- Pore spaces are filled, so water flows overland
Interflow
- Faster than base flow
- Subsurface stormflow
- Aided by macropores
- Also flows along bedrock-soil interface
Flooding
- Rising stage level associated with excess discharge in response to storms or melt
- Natural process that maintains river form and function
- Defined by channel cross-section and bank height
Why is it useful to understand flooding?
- Design of bridges, culverts, sewers, dams, spillways (strength and height of infrastructure)
- Land-use zoning and planning
- Floodplain delineation
- Insurance
Bankfull
- Threshold stage before river flows over banks
- Occurs frequently
What is the probability of a flood happening?
- P = 1/Recurrence interval
What is significant about Q1.5 (a flood recurrence interval of 1.5 years)?
- Most efficient at moving water and sediment
- Maintains channel form and function
- Determined from channel surveys or rating curves
- P~67%
What is significant about Q2.33 (a recurrance interval of 2.33 years)?
- Most common flood discharge
- Useful for delineating floodplain
- P~43%
How do we predict floods?
- Hydrographs
- Recurrence intervals
- Rational Method
Recurrence Intervals
- Annual peak discharge record used to predict flood probability based on record
- R = (number of ranked observations + 1)/m (rank of the observation concerned)
- Can plot a flood frequency curve
Rational Method
- Used when rivers aren’t properly gauged, there is limited historical data
- Relate the unknown area to a similar stream’s behaviour
- Estimates peak annual discharge using empirical formulae and data on rainfall and basin statistics
- Q = 0.278Ci*A
- C = Runoff coefficient
- i = rainfall intesity (mm/hr) at time of concentration t
- A = Basin area
- Hortonian flow is main flow mechanism
Causes of coast flooding
- Storm surges
- Earthquakes
What are factors that influence river floods?
Basin shape, slope, altitude, climate, geology, vegetation cover, infiltration, drainage network factors, channel factors
Why are floods more hazardous in North America?
- Urban growth and infrastructure built in floodplains (not increased flooding)
- BC has some of the largest due to high intensity precipitation and rapid runoff in mountainous rocky terrain