Chapter 08: Streams & Flooding Flashcards
Hydrologic cycle (7)
- Evaporation & transpiration
- Condensation
- Precipitation
- Infiltration & groundwater flow
- Runoff
Rivers of Long Island (5)
- Peconic
- Connetquot
- Stony Brook
- Patchogue
- Carmens
Discharge
volume per time
Q = WDV
Q = width * depth * velocity
*units cubed
Alluvial fan
River that empties out onto land and deposits sediment in a fan-shape because of the drop in velocity
Delta
River that spills out into a body of water via distributaries
Deposits sediments which create the distributaries
Deposit of sediment is sudden because of the drop in velocity
Gaining stream
Water table is saturated and feeding the stream water
Losing stream
Water table is low and the stream is losing water to the water table
Lag time
Time between precipitation event and rise in stream discharge
Lag time decreases as urbanization increases
Effects of urbanization on streams (5)
- Runoff increases
- Infiltration decreases
- Lag time (of flooding) decreases
- Peak discharge increases
- Flooding is worse
Recurrence interval
Helps predict frequency of flooding events
RI = (N+1)/M
RI = (number of years of data + 1) / magnitude or rank of event
Stage
Describes a stream’s discharge status
Stage can be expressed in elevation/height of stream
or
as “flood stage” or “x ft above flood stage”
Natural factors of flooding (3)
- Type of precipitation event
- Ground conditions
- Vegetation cover
Human factors of flooding (4)
- Removal of vegetation
- Destruction of wetlands
- Construction activity
- Urbanization
Flooding reduction methods (4)
- Dams
- Levees
- Channelization
- Retention basins (recharge basins)