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EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct...

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EESC 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack River
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Page 1: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

EESC 2200The Solid Earth System

Flood Case Studies

29 Oct 08

Local hydrograph?

• HW-4 due Wed• no class Mon• no labs next week

Hackensack River

Page 2: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Rain falls: heads to channela Flood

Page 3: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

propagates downstream: Qbalances

Q=dischargecft/sec

QIN

QOUT

a Flood

Page 4: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

propagates downstream: Qbalances

Q=dischargecft/sec QIN

QOUT

a Flood

Page 5: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

propagates downstream: Qbalances

Q=dischargecft/sec QIN

QOUT

a Flood

Page 6: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Discharge (=waterunderbridge)

Discharge

Q =

cross-sectionalareaA

(biggerbridge)

×velocity

V

(fasterriver)

(morewaterunderbridge)

Page 7: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Some channel shapes ......low discharge

high discharge

Aberjona

Charles

Hudson

Area = Width × Depth

Page 8: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Q = A x V

If discharge increases, then have to

• Increase V

• Increase A

--> FLOODS

Page 9: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Discharge varies in 2 ways: Q = A x V

natural

Page 10: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Q = A × V and floods

normal Increase discharge

A increases by river rise, flooding banks

V increases too...

Page 11: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

On big stream systems, discharge increases as tributaries bring in more water

Q, A and V all increase!!

Page 12: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Flood plain

Page 13: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Natural systems havefloodplains, why?

1. Water speedfaster farther frombottom

2. Faster watercarries bigger load

slow

fast

clay gravelgrain size

speederosion

transportdeposition

Page 14: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

slow,deposition

Why: stream erodes channel,fills floodplain

fast,erosion

Page 15: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Flood Case Studies

1.Hurricanes and Deltas2.Big Thompson Canyon3.1993 Midwestern Flood4.100 yr floods5.Ancient tales of floods6.Channel scablands

• When• Where• Deaths• $$ Damage• How Big?• Problems• Mitigation?

Page 16: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Hurricanes and Deltas

Page 17: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Bangladesh

Page 18: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Living in Bangladesh

Page 19: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

New Orleans

Page 20: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack
Page 21: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Big Thompson Canyon

Page 22: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Big ThompsonCanyon, CO

Page 23: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack
Page 24: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

1993 Midwestern Flood

Page 25: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

dark blue -- flooded in 1993

Saint Louis

Page 26: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

JeffersonCityMO

Page 27: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Tuttle Ck spillway, KS: 24 Jul 93, 35000 cfs

Page 28: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

The1993Flood

ExcessRainfall

>200%

StLouis

Page 29: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Affected a large areaRainfall causes flooding in “streams”

Page 30: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

St.LouisGauge

PreviousRecord

FloodStage

Page 31: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

What happened? 1. Fall before, heavy rains saturated soils

2. Unusual summer jet stream

normal summer 1993

cool, dry air

warm, moist air

H

p. 386

Page 32: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

1993 Overall: Worst flood in US history

$20 billion damage 50,000 homes damaged 75 towns submerged 48 fatalities

peak discharge = 1,030,000 cft/s at St Louis

Page 33: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

18Jul93

Page 34: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Discharge varies in 2 ways: Q = A x V

natural

same sizeLevee

not

higher V

high V

Page 35: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

100 yr floods

Page 36: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Flood recurence intervals: Q vs rate Data: # peak floods > Q

in last (10, 50, 100) years?

Extrapolate to get rate of “100 yr” flood

020000400006000080000

100000120000140000160000180000

1 10 100

average recurrence

Q:

Dis

char

ge c

ft/s

?

19931974

Page 37: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Ancient tales of floods

Page 38: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

JohnMartin.TheDeluge.1834.Oiloncanvas.66x102inches.

Page 39: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Same story in many mid-eastern culturesOldest: Gilgamesh, 1st epic literature

(Sumeria, 2000 - 3000 BCE)Did something actually happen?

Page 40: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Traditional Idea: flood Tigris,Euphrates (“1000 yr flood”)

Gulf

Problems: not that much water here

no giant flood deposits

Page 41: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack
Page 42: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Black Sea...

Bosporus St

Mediterranean

Black Sea

Page 43: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Shallow Strait of Bosphorous

NSMedit.Sea Black Sea

45 m bsl

salty fresh

last Ice Age

p. 396

Page 44: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

salty fresh

Shallow Strait of Bosphorous

NSMedit.Sea Black Sea

5600 BC

Page 45: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

In Black Sea...

• 5600 BCE: sudden deluge• change from fresh -> saline• scouring of Bosporous channel

– 80 - 100 km/hr flows?– Black Sea level rises 100 m in 1 year?– Major flood of Black Sea shorelines...

Page 46: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Conclusion

Catastrophic flooding at 5600 BCEalso, 4 Ma flooding of Medittteranean

Displaced humans: probably

The Great Deluge?

Page 47: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Channel scablands

Page 48: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak Chapter 17: Streams and Floods: The Geology of Running Water

Page 49: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak Chapter 17: Streams and Floods: The Geology of Running Water

Page 50: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

Flood Forecasting

• rainfall• saturation

Page 51: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

available water = watershed area × rainfall

-> big watersheds (Mississippi) more potential

Flood Factors

Time Lag between rain and flood

1.

2.

time, hrs

rain

dischargeamount

Page 52: EESC 2200 • HW-4 due Wed The Solid Earth … 2200 The Solid Earth System Flood Case Studies 29 Oct 08 Local hydrograph? • HW-4 due Wed • no class Mon • no labs next week Hackensack

SummarySummary

• Flood = high Q over banks

• Causes: rainfall, ground saturation

• Lag and duration: Drainage Basin size

• Urbanization, levees intensify floods


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