![]()
GES 101 Handout: Surficial Water
Distribution of H20 on Earth
-1.36 billion km3 H20 near surface
Volume
Oceans 97.3%
Glacier & Polar Ice 2.1-3.5%
Underground Aquifers 0.6%
Lakes & Rivers 0.0160%
Atmosphere 0.001%
Biosphere 0.00004%
Streamflow
Hydrologic Cycle: describes quantity and distribution of H20 on Earth's surface.
channelized flow of any size
Stream- dominant agent of landscape alteration = 40% of rainfall "runs off" (=60% infiltrates or soaks into the ground)
Discharge = (avg. current velocity *cross-sect. area of stream)
A stream's discharge, velocity and depth all increase downstream
Laminar vs turbulant flow
Stream cross-section and longitudinal profile
local (temporary) Base level
- ultimate base level= sea level
Graded stream is in "equilibrium"
"lifting"
Stream erosion
abrasion
dissolution (limited)
In the U.S. the erosion rate is 461 tons/yr per square mile.
Sediment Transport
-suspended load: clay and silt
-bed load: sand, pebbles and boulders
-dissolved load (average is about 200 ppm)
Stream Deposits are made of alluvium
-channel bars
-channel deposits
-point bars
-braided patterns
-deltas
-alluvial fans
-fan deltas
-depositional flood plains
-natural levees
-meander scars
Meanders
-oxbow lakes
-artificial cutoffs
Stages of stream development
youthful
mature
old age
Drainage Networks
-drainage basins
-divide
drainage patterns
-dendritic
-radial
-rectangular
-trellis
Antecedent vs. Superposed streams
water gaps
Headward Erosion and Stream Piracy
wind gaps
Stream rejuvination -> entrenched meanders
Stream Terraces -erosional vs. depositional
-paired = same age
-unpaired = different ages
Flood hazard
-most common and costly hazard in U.S.
-most human activity aggravates flood hazard
Bankful Stage = Bankful discharge
Flood Frequency - statistical prediction
Hydrograph: fluctuation in stream discharge over time -- info. on "normal" stream behavior
Recurrence Interval (RI) = (N+1)/m
Annual Exceedence Probability = 1/R.I.
Flood Frequency Curve
Effect of Urbanization on discharge:
-magnitude of flooding increases
-frenquency of flooding increases
-shorten lag time between rainfall and flood
Adjustments to flooding
1. Control flood - dams, levees, cloud seeding
2. Decrease physical vulnerability - forecasting warning system & evacuation
3. Spread costs - govt. relief (subsidized insurance; in 1981, the annual subsidy for those homes located in floodplains was $231).
20's and 30's - structural solutions
40's and 50's - societal adjustments (insurance)
1968 Natl. Flood Ins. Act negligible participation
1973 Flood Disaster protection Act -"mandatory" -River Flood Mapping
Review Questions: Running Water
Back to 101 Home Page Back to Handouts Page
![]()