Surface Water 2 - Overland Flow Flashcards

1
Q

Overland Flow

A
  • Non-Channeled water flow on ground surface
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2
Q

Factors that influence overland flow

A
  • 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)
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3
Q

Types of surface runoff during rainfall or snowmelt

A
  • Infiltration excess overland flow (Hortonian)

- Saturation excess overland flow

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4
Q

Hortonian overland flow

A
  • 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
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5
Q

Saturation excess overland flow

A
  • Occurs when soil becomes saturated and there is no longer any space for water to infiltrate
  • Pore spaces are filled, so water flows overland
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6
Q

Interflow

A
  • Faster than base flow
  • Subsurface stormflow
  • Aided by macropores
  • Also flows along bedrock-soil interface
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7
Q

Flooding

A
  • 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
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8
Q

Why is it useful to understand flooding?

A
  • Design of bridges, culverts, sewers, dams, spillways (strength and height of infrastructure)
  • Land-use zoning and planning
  • Floodplain delineation
  • Insurance
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9
Q

Bankfull

A
  • Threshold stage before river flows over banks

- Occurs frequently

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10
Q

What is the probability of a flood happening?

A
  • P = 1/Recurrence interval
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11
Q

What is significant about Q1.5 (a flood recurrence interval of 1.5 years)?

A
  • Most efficient at moving water and sediment
  • Maintains channel form and function
  • Determined from channel surveys or rating curves
  • P~67%
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12
Q

What is significant about Q2.33 (a recurrance interval of 2.33 years)?

A
  • Most common flood discharge
  • Useful for delineating floodplain
  • P~43%
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13
Q

How do we predict floods?

A
  • Hydrographs
  • Recurrence intervals
  • Rational Method
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14
Q

Recurrence Intervals

A
  • 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
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15
Q

Rational Method

A
  • 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
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16
Q

Causes of coast flooding

A
  • Storm surges

- Earthquakes

17
Q

What are factors that influence river floods?

A

Basin shape, slope, altitude, climate, geology, vegetation cover, infiltration, drainage network factors, channel factors

18
Q

Why are floods more hazardous in North America?

A
  • 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