Sem#2 Chap 5 Flashcards

(120 cards)

1
Q

Inland floods in non-coastal regions result from:

A
  • Oversupply of rainfall
  • Oversupply of melting snow
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2
Q

Stream floods:

A
  • When water spills over the banks of a stream channel
  • Most inland flooding results from stream flooding.
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3
Q

Areal floods:

A
  • When low areas collect water and become submerged
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4
Q

Urban floods:

A
  • When cities are inundated due to insufficient drainage
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5
Q

Floods also occur when _____
and ______fail.

A

dams and levees fail.

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6
Q

Hydrologists:

A
  • Scientists who study water on and below the land
  • Distinguish between flood types
  • Research stream discharge, competence, and capacity
  • Use spatial data to create flood probability maps
  • Use models to predict flood interval probabilities
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7
Q

Slow-onset floods (development time)

A
  • Develop over days or weeks
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8
Q

Flash floods (development time)

A

Develop over minutes or hours

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9
Q

Runoff:

A

water flowing from an area in response to gravity

  • Overland flow: water flows across land as a thin layer (sheetwash).
  • Stream flow: water flows down a trough or channel.
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10
Q

Stream

A

any flowing body of water in a channel
* Medium-sized streams are called creeks or brooks.
* Large-sized streams are called rivers.

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11
Q

Streams form when ?

A

runoff carves a trough into the ground.
* Downcutting deepens stream channels.
* Headwater erosion lengthens stream channels.

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12
Q

Slide #5 Chap #5

A

Slide #5

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13
Q

Headwater

A

where a stream begins to flow

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14
Q

Mouth

A

where a stream empties into another body of water

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15
Q

Gradient

A

a stream’s slope, in the downstream direction

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16
Q

Longitudinal profile:

A
  • Plots elevation on the vertical axis
  • Plots distance from mouth on the horizontal axis
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17
Q

Floodplains

A
  • Wider than stream channel
  • Submerged during a flood
  • Often contain fertile soil
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18
Q

Base level:

A
  • The elevation below which a stream surface will not drop
  • Local base levels lie upstream from mouth.
  • Lakes and tributaries are local base levels.
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19
Q

Stream flow creates ______ and dissolves _______.

A

sediment and dissolves minerals.

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20
Q

Dissolved load

A

mineral ions in solution

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21
Q

Suspended load

A

silt and clay particles within a stream

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22
Q

Competence

A

the maximum clast size a stream can carry
* Faster flowing streams have greater competence.
* Muddy (denser) streams have greater competence.

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23
Q

Capacity

A

the total quantity of sediment a stream can carry
* Competence and water Alluviumvolume dictate capacity

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24
Q

Alluvium

A

a layer of settled stream sediment

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25
Coarse alluvium settles from _______
faster-flowing streams
26
Fine alluvium settles from __________
slower-flowing streams
27
Bar
an accumulation of gravel and sand along or within a channel
28
Alluvial fan
a wedge of sediment deposited at a canyon mouth
29
Floodplain deposits consist largely of _____ and _______.
largely of silt and clay.
30
Natural levees
* Sediment ridges on the banks of a stream channel * Form as water slows and spills into a floodplain
31
Deltas
* Sediment wedges at the mouth of a stream * Form as water empties into a standing body of water
32
Distributaries
* Small channels cutting across a delta
33
Delta plains
are broad lowlands liable to flooding.
34
Permanent Streams
 Fed by sufficient overland flow, tributaries, and springs  Stream bed remains submerged  Water table lies above stream bed  Common in temperate and tropical regions  Flow all year
35
Ephemeral Streams
 Fed by insufficient overland flow, tributaries, and springs  Stream bed is often exposed  Water table lies below stream bed  Common in semiarid and arid regions  Flow only part of the year  Dry wash/arroyo/wadi: a completely dried up ephemeral stream
36
Meandering Streams
Often flow across broad floodplains with deep alluvium May carve meandering canyons: * Base level must drop relative to land surface. * Stream downcuts into bedrock.  Course changes are common: * Water flows faster on outer curves, creating cut banks. * Water flows slower on inner curves, creating point bars. Oxbow lakes form when a meandering neck is eroded away.
37
Evolving Meanders
A channel’s position changes within a floodplain as meanders evolve.
38
Meandering River
river with a single channel and high to moderate sinuosity.
39
Cutbanks (CB)
form on the outside of meander bends where the water is accelerated along the outside wall and erodes into the bank.
40
Point bars (PB)
form as sediment is deposited in the slower water on the inside of the meander bends.
41
Thalweg
the deepest parts of the channel along the length of the stream bed
42
 Evidence of channel position changes:
* Abandoned meanders, relict point bars, and oxbow lakes
43
Braided Streams
 Carry large quantities of sediment when flow is high  When flow slows, sediment settles into elongated bars.  Stream separates into small channels flowing around bars.  Channels resemble braided hair.
44
Braided River
a river characterized by multiple, frequently shifting channels. * Common in regions where there is a strong seasonally and monthly variation in stream discharge * During short periods of high discharge a braided river carries the coarsest sediment * Develop in regions where sediment is readily available
45
Watershed
the land area from which water drains * Also called catchments or drainage basins
46
Watershed tributaries feed water into a ______.
trunk stream
47
Trunk stream drains water from ______.
watershed
48
Drainage network includes:
* Watershed’s tributaries * Watershed’s trunk stream
49
Drainage divide
* Elevated land separating drainage networks
50
Continental Divide
* Separates drainage networks flowing into different oceans
51
The Amazon Drainage Network
 The largest drainage network in the world  Drains much of South America  Continental divide follows the crest of the Andes
52
1st-order streams:
* Small streams * No tributaries * Near margins of drainage network
53
Low-order streams drain _____ areas
small
54
High-order streams drain _____ areas.
large
55
Two 1st-order steams merge to form a 2nd-order stream
(just a knowledge thing, repeat for every #stream take 2 to from the next)
56
 A trunk streams is a network’s _______
highest-order stream.
57
Stream Discharge
The water volume passing a cross-sectional area
58
 Cross-sectional area
* A plane drawn perpendicular to the banks of the stream
59
 Cross-sectional area formula
𝐷𝐷 = 𝐴𝐴 × 𝑣𝑣 * D = discharge * A = cross-sectional area * v = average water velocity Reported in m3 or ft3 per second
60
Gauging stations
record stage and average velocity.
61
Stage
* A reference elevation just below the streambed
62
Temperate and tropical places(Discharge Variations):
* Tributaries and springs add water to flow. * Discharge often increases downstream.
63
 Arid and semi-arid places(Discharge Variations):
* Water seeps into ground, evaporates, or is removed. * Discharge often decreases downstream.
64
Trunk stream discharge (what does it represent)
* Reflects watershed size and climate
65
Turbulence develops from ________
shearing water flows
66
(Discharge Variations): Calculations are inexact due to _________
friction and turbulence.
67
Flood stage:
* When water rises above a stream bank * Significant areas outside channel are submerged. * Cross-sectional area and average flow velocity increase.
68
Large elevation increase in flood stage:
* When stream channel lies within a narrow valley
69
Small elevation increase in flood stage:
* When stream channel lies within a low-lying floodplain
70
Discharge changes during a flood.(increase and decrease explain)
* Increases as flood develops * Decreases as flood recedes
71
Discharge resembles a ________
bellshaped curve
72
Peak discharge:
the highest point on a hydrograph
73
Flood crest:
when water reaches highest stage
74
Lag time is the difference between:
* The event triggering flooding * Flood crest
75
Slow-Onset Floods
 Water rises for days or weeks.  Water recedes over weeks or months.  Affect high-order trunk streams in downstream places  Hydrographs display wide curves.  Common in Bangladesh, within the Ganges River Delta  ~80% of Bangladesh’s people live on the Ganges River Delta.  Flooding requires millions of people to evacuate
76
Flash flood characteristics
* Discharge becomes hazardous in < 6 hours. * Discharge increases after a short lag time. * Floodwaters quickly recede. * Affect small areas * Affect low-order streams
77
Hydrographs have a _______
narrow, bell-shaped curve
78
Flash Flood Dangers
 People and motorists are often caught by surprise.  Water may flow faster than people can run or drive.  Helicopters may be required to save people.  Turbulent water causes rapid erosion.  Dynamic pressure of sedimentladen water destroys structures.  Heavy debris batters and buries areas downstream.
79
Rapid melting snow may cause ________
flash floods * Spring rain melts winter ice. * Volcanic eruptions melt glaciers and snow caps.
80
Ice dams:
natural walls of ice holding back water
81
Outburst floods result when ______
ice dams fail
82
Iceland’s “Jökulhlaup” floods:
* Meltwater accumulates beneath a glacier. * Outburst flood results when water breaches glacial toe.
83
Glacial Torrents
Immense outburst floods from melting glaciers
84
Ice Jams
 Form when river ice breaks up during the spring  Ice encounters an obstacle and piles up.  Ice blocks water from flowing downstream.  Water floods into floodplain.  Outburst flooding may result when ice jam breaks
85
Areal Flooding
 Land is submerged due to heavy rain or rapid snowmelt.  Flooding occurs without input from a nearby stream.  May delay agricultural planting  Farmland and low-lying communities at risk
86
Urban Flooding
A flood that inundates a built environment  May occur during slow-onset and flash-flood events  Flood control channels may expedite water removal.
87
Urban Flooding: Two causes:
Impermeable surfaces that prevent water infiltration * Inadequate drainage
88
Urban Flooding: Potential impacts:
* Toxic runoff causing environmental damage * Higher flood crest
89
Before urbanization
* Rainwater infiltrates the ground. * Less discharge, and peak occurs after a long lag time
90
After urbanization:
* Rainwater flows directly into streams. * More discharge, and peak occurs after a short lag time
91
Artificial Levees
 Constructed ridges of gravel, sand, and compacted clay  Built along a stream to confine flow to main channel  Prevent flooding along many river channels  Vulnerable to accidental or deliberate damage * Military conflicts may intentionally damage levees.
92
Artificial Levees: Construction parameters
Construction parameters: * Base should be 3 times wider than height * May be built atop natural levees
93
Levee Failure: Overtopping
Occurs when water rises high enough to flow over a levee * Water velocity and volume increase. * Erosive power increases as water flows over levee. * Water may scour a channel in levee wall.  May also occur due to: * Tree roots disturbing soil * Floating debris colliding with levee wall * Slumping in levee wall
94
Levee Failure: Underseeping
 Also called undermining  Water pressure difference: * May force water through levee base * May force water through sediment beneath levee  Fountaining may develop: * Water flows through narrow pathways beneath levee. * Sand volcanoes may appear.  Fountaining indicates that a breach is imminent.
95
Levee Failure: Structural Damage
 Structural weakness may be caused by: * Bad concrete * Poorly compacted clay * Weak foundation  Concrete barriers may crack.  Levee foundation may shift.  Slumping may occur on either side of levee.
96
Danger Due to Moving Water
 Driving across flooded roads can be fatal.  Water’s dynamic pressure rises with the square of its velocity.  Even shallow water can easily push vehicles sideways.  Buoyancy force pushes vehicles upward.  Flash flood casualties result from people trapped in cars.  Debris in floodwater often destroys bridges and buildings.  Floodwaters erode riverbanks.  Floodwater alluvium may bury streets and buildings.
97
Damage Due to Rising Water
 Floodwaters may submerge fields, homes, and businesses.  Transportation and communication networks fail.  Animals drown if unable to escape to higher ground.  Power generation fails, so electricity goes out.  Floodwater residue contains garbage, sewage, and chemicals.  Mud and silt muck are left behind as water recedes.  Secondary disasters of cholera and dysentery are common.
98
Monsoon
* A seasonal reversal in wind direction * Wind reversal causes shift in precipitation.
99
South Asia’s intense monsoonal rainy season:
* Intertropical convergence zone (ITCZ) drifts north. * Indian Ocean moisture spawns heavy rains.
100
Atmospheric rivers:
* Narrow bands of moist air flowing inland from Pacific ocean * Air flows along the south side of a mid latitude cyclone.
101
 Recurrence interval:
Average years between two floods of a given discharge or greater
102
How to calculate Recurrence Interval
𝑅 = (𝑁/1)÷ 𝑀 * R: recurrence interval * N: number of years of flood records * M: rank of flood, with largest ranked #1
103
Hydrologists prefer using ____ to report flood likelihood
AEP
104
AEP determines likelihood of:
* A flood of a given discharge or greater will occur in a given year * AEP is reported as a percent.
105
AEP Formula
𝐴 = (1÷𝑅)𝑥100
106
Flood Frequency Graphs: Show Relationship Between
* Recurrence interval * Peak discharge
107
Lower-discharge floods: (flood graphs)
* More frequent recurrence * Plot in graph’s lower left
108
Higher-discharge floods:(flood graphs)
* Less frequent recurrence * Plot in graph’s upper right
109
Climate change will modify:
* Recurrence intervals * Frequency curves
110
National Weather Service (NWS) officials:
* Track severe weather * Keeping public informed of potential flooding
111
Flash flood watch:
* Conditions may lead to flooding within 12–36 hours
112
Flash flood warning:
Flooding has been detected.
113
River flood warnings:
* Issued when large rivers are expected to reach flood stage
114
Predicted Flooding Risks Correlated
Minor: Low ground flooded, and low parts of roads underwater; no internal house flooding (maybe a few basements); water over roads won’t stall vehicles Moderate:Numerous buildings flooded; some infrastructure affected; some people need evacuation; water makes roads impassable. Major:Houses destroyed or floated off foundations; infrastructure destroyed; bridges washed away; severe erosion; extensive evacuations; National Guard generally called in.
115
Protecting Communities from Floods
 Sandbagging can reinforce and increase levee height. * May increase flooding risk for downstream areas  Additional efforts: * Constructing diversion canals * Restoring wetlands * Passing laws that prohibit construction in floodways  Adding sandbags to a levee to increase its height
116
Private flood insurance is ______ available
rarely
117
National Flood Insurance Program:
* Provided by the U.S. federal government * Premiums are expensive
118
Federal buyout programs:
* Purchasing flood-prone land for parks or wetlands
119
Community wealth:
* Poor communities often grow in flood-prone areas. * Building homes on stilts may be possible for some people.
120
Floodway zoning ensures _____
minimal losses from a flood