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SEA LEVEL CHANGE AND TRANSPORTATION PLANNING
byBob Dean
University of Florida
SEA LEVEL CHANGE AND TRANSPORTATION PLANNING
byBob Dean
University of Florida
Questions to Address
(1) What is the Long-term History of Sea Level Change?(2) Is Global Sea Level Currently Rising? If so, What is the Rate?(3) Is Global Sea Level Accelerating? If so, What is the Rate?(4) Prognosis for Future Sea Level Rise Rates. (5) Relevance to ransportation System Design
Questions to Address(The Engineering Response)
(1) Incorporate Effect in Initial Design(2) Retrofit at Some Future Time
An Afterthought: Possible Role of Sunspots on Global Climate Change
Relative Sea Level Rise: Definitions
Relative Sea Level Rise (RSLR) = Global Sea Level Rise + Local EffectsGlobal = EustaticLocal = Tectonic + Compaction + Post Glacial Rebound + Subsidence + …….
Components of Eustatic SLR
(1)Thermal expansion of water(2) Alpine glaciers(3) Ice Sheets: Greenland, and Antartica
Sea Level Change Over the Last 500 Million Years
Sea Level Change Over the Last 1 Million Years
Sea Level Rise Over the Last 24,000 Years
Sea Level Rise Over the Last 8,000 Years
World Wide Distribution of Long- Term Tide Gages
Relative Sea Level Change Based on Tide Gage Data
RSL Change: Juneau, AKAn Example of Post Glacial Rebound
RSL Change: Adak, AKNote Tectonic Effects
RSL Trends in AlaskaStation Trend (mm/year) Period Of Analysis
Adak -2.63 1957 - 1999
Anchorage + 2.67 1972 – 1999
Cordova + 6.97 1964 – 1999
Juneau -12.69 1936 – 1999
Ketchikan - 0.11 1919 – 1999
Kodiak - 12.08 1975 – 1999
Nikiski - 10.71 1973 - 1999
Sand Point + 0.07 1972 – 1999
Seldovia - 9.03 1964 – 1999
Seward - 1.46 1964 – 1999
Sitka - 2.17 1938 – 1999
Skagway - 12.69 1936 - 1999
Unalaska - 6.44 1957 – 1999
Valdez - 0.34 1973 – 1999
Yakutat - 5.75 1940 - 1999
Subsidence
• Subsidence can be substantial exceeding the eustatic component significantlyLong Beach, CA: > 6 m due to hydrocarbon extractionTokyo: 3.5 m due to water extractionOsaka: > 2 m due to water extractionCoastal Louisiana: Up to 1 m per century due to natural and anthropogenic causes
Subsidence Due to Natural and Human Causes
Production Rates and Bottom Hole Pressure Reduction. Valentine Oil Field, LA
a) Production Rates of Oil, Gas and Water
b) Reduction in Bottom Hole Pressure
Eustatic Sea Level Rise Estimates
Sea Level Rise Rate (mm/yr)
Years No. of Tide
Stations
Investigators
1.43 1881-1980 152 Barnett2.27 1930-1980 152 Barnett1.2 1880-1982 130 Gornitz &2.4 1920-1970 40 Peltier &
1.75 1900-1979 84 Trupin & 1.8 1880-1980 21 Douglas, et al
1.62 1807-1988 213 Unal &
Average Sea Level Rise Over the Last 120 Years
Is Global Sea Level Rising?
Yes. Over the Past Century, the Rate Has Been Between 1 and 2 mm/year (I Like 1.2 mm/year).A Caveat: Most Tide Gages Are Located Near Areas of Ground Water Extraction. Effect on Gage Readings?
Is Sea Level Rise Accelerating?R
ate
of C
O2 I
ncr
ease
, M
aun
a L
oa, H
I
Average Global Temperature Change
Some Predictions and Considerations of Future Sea
Level Rise, 1980’s
Sea Level Rise Projections (IPCC)
Long-term Eustatic Rate
Is Sea Level Accelerating?
Long Term
RSLR at Several
Locations
IPCC Estimates of Future SLR
Date of IPCC Prediction
Time Period (Years)
IPCC Sea Level Rise
Ranges
IPCC Mid Range Estimate
1995 1990 to 2100
15 cm to 95 cm
50 cm
2001 1990 to 2100
8 cm to 88 cm 49 cm
Probabilities of Sea Level Rise:2000 to 2200
Is Sea Level Accelerating?
(1) There are Indications of Sea Level Acceleration Although They Are Weak and do not Appear to be Increasing(2) Probably Won’t Know About Anthropogenic Effects Definitively for 30 or More Years
Will Sea Level Rise Accelerate in the Future?
Probably, However, the Timing and Rates are Extremely Uncertain
As Support, the Predicted Rates of Acceleration Have Decreased Since 1984 When Some Early Predictions Started
Engineering Responses
* Some Highways: Increase Protection as Need Becomes Apparent* Bridges and Other Infrastructure Less Suited for Retrofitting: Allow for RSLR in Original Design
Example/DiscussionCoastal Highways
* Base design on predictions of local RSLR* Usually, not readily retrofitted during design life* Flooding of special concern if evacuation route* If evacuation route, design for upper limit of probabilities
Example/DiscussionRevetment Protecting a Coastal Highway
* Several coastal engineering options for retrofitting during design life, including
* Adding more and heavier armor units
* Beach nourishment to reduce size of waves
Summary
• Sea level has changed over millions of years under natural forcing
• Current rates of eustatic sea level rise are between 1.2 to 2.0 mm/yr
• There is not consensus of an acceleration of eustatic sea level rise nor of the role of human activity
• Transportation and design should understand coastal engineering options for retrofitting during design life
• Transportation planning and design should include local relative sea level rise if critical to the performance
Possible Role of Sunspots in Eustatic Sea Level Rise
Solar Forcing and Glaciation Stages
Su
nsp
ot H
isto
ry:
1700
to
2006
Recent Sunspot Activity
Correlation Between Sunspot Numbers and Solar Flux
Yearly Sunspot Numbers:1610 to 2000
Reconstructed Temperature:0 to 2000 AD
(Note “Little Ice Age” Period)
QUESTIONS?
Example of Acceleration Concerns of Sea Level Rates (1983)
Is Sea Level Rise Accelerating?
Consider:
and evaluate a and b from the data on the following slide. b is an acceleration term.
dSa bt
dt
Is Sea Level Rise Accelerating?
This leads to: dSa bt
dt
Where t Is the average of the time period over
which is determined. Solving for
a and b from the data yields very unrealistic results signifying that the data are not well conditioned for this purpose.
dS
dt
Engineering Response
NRC Report (1984)
“The Prognosis for Sea Level Rise Should Not be a Cause for Alarm or Complacency”
Measurement of Sea Level Change
Outline
(1) Definitions(2) Discuss Magnitudes of Relative Sea Level Rise(3) Is the rate of sea level rise increasing(4) Engineering responses to sea level rise (NRC Report)
Examples of Subsidence Due to Ground Fluid Extraction
Location Cause of Subsidence Characterization of Subsidence
Terminal Island, CA Hydrocarbon Extraction > 6 m
Tokyo, Japan Ground Water Extraction > 4 m
Osaka, Japan Ground Water Extraction > 2 m
Coastal Louisiana Natural Compaction and Extraction of Hydrocarbons
Up to 1 m/year