VOCAB GHC Ch 13: Floods Flashcards
Regional floods
Huge, long-lasting floods in large river valleys with low topography resulting from prolonged heavy rains over an extensive region. They cause heavy economic losses.
Flash Flood
A local and sudden flood of relatively great volume and high velocity that lasts for a short time following a few hours of intense rainfall. Flash floods cause many deaths.
Gradient
The slope of a stream channel bottom; change in elevation divided by distance. Gradient increases with steeper slope.
Base level
The lowest point to which a stream or river can flow, often referred to as the ‘mouth’ of the river; usually sea level.
Equilibrium
A state of balance in a system; a condition in which opposing processes are so balanced that changes cause compensating actions.
Discharge
The volume of water flowing in a stream per-unit of time.
Sinuosity
The length of a stream channel divided by the straight-line distance between its ends.
Load
The amount of material moved and carried by a stream.
Meander
The curves, bends, loops, and turns in the course of an underloaded stream that shifts its bank erosion from side to side of its channel.
Braided stream
And overloaded stream so full of sediment that water flow is forced to divide and recombine in a braided pattern.
Graded stream
An equilibrium stream with an evenly sloping bottom adjusted to efficiently handle water flow (discharge) and sediment (load) transport.
Floodplains
The nearly flat lowlands that border a stream and act as the stream bed (the physical confine of the normal water flow) during floods.
Feedback
A change in the system that provokes further changes.
Positive feedback
Occurs in nonequilibrium systems where one changed triggers more changes in the same direction. The vicious cycle.
Negative feedback
Occurs in equilibrium systems where one change triggers another change that tends to negate the initial change and restores equilibrium. Example: when too much water pours into a channel, increased erosion lowers the gradient to slow the water flow and maintain equilibrium.
Recurrence intervals
The average time interval between floods or earthquakes of a given size.
Avulsion
The abrupt change in the course of the stream and the adoption of a new channel.