Chapter 2 Flashcards
Hydrologic Cycle
The local, regional, and global movement of water in all three phases (gas, liquid,
solid)
Watersheds
A land area from which all water drains to a single point, called the watershed outlet, bounded by a ridge
Channel Heads
Higher elevation locations where small stream channels start
Channels tend to be ____ near their heads and ____ near their outlets
inside narrow, steep valleys
inside broader, flatter areas
Floodplain
The land area that is covered in water during a flood
Factors that can affect potential flooding
Soil infiltration capacity, soil thickness, slope steepness, amount of water in the soil, and amount of vegetation on the land surface
Which types of soil are able to absorb rainwater faster?
Coarse (sandy), as opposed to fine (clayey)
Flash Flood
Sudden flooding that typically occurs in the headwater portions of a watershed where slopes are very steep, leading to very rapid surface runoff
What typically causes a flash flood?
Intense rainstorms centered over small sub-watersheds, dam failures, sudden breaking of debris jams, or landslides into water bodies
Downstream Flood
Floods generally produced by rainstorms of a wide extent and long duration. They occur at lower portions of a watershed, and the runoff from large parts of the watershed may take a long time to arrive, causing the flood to develop relatively slowly. The slope in downstream channels is also flatter, which will also cause the water to move slower
Pro and con to downstream floods
Pro: allows for ample warning time
Con: slow to recede, leading to long disruptions and damage
Flow Rate or Discharge
The volume of water flowing past a point per unit time (typically cubic meters per second or cubic feet per second)
Hydrograph
A plot of flow rate versus time, showing the progress of a flood
Flood Frequency
The probability that a flood of at least a certain size will occur in any particular year
Recurrence Interval of Floods
The average time (usually years) between floods of a certain size, also the mathematical inverse of frequency
Types of damage caused by floods
Damage caused by currents, debris, and sediment
Erosion and deposition of sediment
Pollution of rivers
Hunger and disease
Damage caused by currents, debris, and sediment
Floods may leave in their wake tremendous damage to infrastructure (particularly transportation due to damage to bridges). Many people potentially are made homeless by destruction of their residences.
Erosion and deposition of sediment
Floods often cause severe erosion, with
the consequence that formerly productive farmland can be degraded. The eroded sediment that is deposited elsewhere can be damaging in many ways.
Pollution of rivers
Many pollution-laden structures and facilities (wastewater treatment plants, petroleum storage tanks, etc) are located in floodplains. A serious flood can damage the structures, releasing various types of pollutants into the river system.
Hunger and disease
Pathogens are likely to be carried into stream systems by floods. If those streams are used for water supply, disease outbreaks are possible. The damage to farmlands and the general disruptions of major floods can trigger food shortages and famine.
Urbanization and Flooding
Urban areas are dominated by pavement and other impervious surfaces that are
unable to absorb waters. The surfaces are also relatively smooth, causing the surface runoff to travel much more quickly than it would on vegetated surfaces. Additionally, many urban areas are drained by storm drains which further accelerate the transport of rainwater to stream, increasing the flood risk. Bridges and other structures built in the vicinity of streams also created the possibility of flooding related to debris jams.
Flood damage control methods
Dams, levees, channelization, site improvements, and land use planning
Dams
A reservoir space that can temporarily stored flood water, and release it slowly over a long period of time. The same total amount of water eventually flows downstream, but the peak flow is much reduced, hopefully to a level that does not exceed bankfull downstream. Dams are also expensive to construct and difficult to maintain.
Possible dam failures
Landslides into the reservoir, erosion of the dam foundation during a flood event, extreme amounts of flood water over-topping the dam, and earthquakes