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June 23, 2016
The History of Coastal Flood
Hazard Assessments in the Great
Lakes
Brian A. Caufield, P.E.,
CFM
The Great Lakes
2
Some Statistics
 Courtesy of Great Lakes Information Network
 One-fifth of the world’s fresh surface water
 Spread out over the contiguous U.S., would submerge the
country under 9.5 feet of water
 More the 94,000 square miles (larger than New York, New
Jersey, Connecticut, Rhode Island, Massachusetts, Vermont,
and New Hampshire combined)
 10,900 miles of coastline (U.S. and Canada combined)
 3,288 miles in Michigan (only Alaska has more)
3
4
Just because an inland body of water doesn’t
make it immune to risk
 Fast moving squall lines can create localized risks
 Passage of low pressure centers act similar to hurricanes
 Central pressures recorded similar to those of a tropical or extra-
tropical storm
 Storms can create:
 Surge
 Waves
5
Generalized Coastal Zone Schematic
Wave Runup
Kennedy, Layne. 2010. September 4, 2014. http://laynekennedy.blogspot.com/2010_10_01_archive.html
Overtopping
Green, M. Spencer. AP Photo. 2012. September 4,2014.
http://journalstar.com/ap/business/two-story-waves-on-great-lakes-halt-shipping/article_bcf2bb34-b528-52f5-8cd4-0c57e7ea8922.html
Overtopping
Jackson, Brian. North Ave. Beach. 2012. September 4, 2014.
http://www.suntimes.com/photos/galleries/index.html?story=16046778
Overland Wave Propagation
Unknown. Flooding in Green Bay, WI. 1973. September 4, 2014.
http://greatlakesresilience.org/stories/wisconsin/nor%E2%80%99easter-coastal-storm-flooding-green-bay
Early attempts to identify flood risks
11
Waves and Erosion
 Waves
 Leverage USACE Wave Information Study (WIS) 1956-1987
 Local wave height with recurrence interval of 3 years approximately
describes wave action likely to accompany the base flood
 ½ year was used on Lake Ontario due to a different fit for the wave
data on the lake
 Erosion
 Based on FEMA (1989)
 Erosion (in square feet) = 85.6 * Recurrence Interval (in years)
 270 square feet for 3-year recurrence
 190 square feet for 2-year recurrence
12
2009 Update
1. Return period lake level
recommended on a
USACE (1988) report, but
additional 20-years of
observations
2. Wave runup is dominant
risk and a response based
approach is desirable
3. Previous wave guidance
included long-term lake
processes
13
Updated Water Levels
14
Combination of Water Levels and Waves
15
Great Lakes Coastal Flood Study
 Kicked off in 2009
 Basin-wide assessment of flood risks
 Updated Guidance
16
Crosswalk
December 1990 Storm
Overall Process
Offshore Waves Still Water Level Levels
Wave Transformation
If Necessary
Flood Hazard Mapping
Wave Height
Wave Crest Elevation
Wave Runup
Wave
Overtopping
Erosion
Shoaling Zone
Surf Zone
Backshore Zone
Coastal Structures
Wave Setup
Study Approach
 Regional Study Approach
 Water level and wave analysis
 Improvement over community-
county
 Reduces number of boundary
conditions
 Greater consistency in
assumptions
 Local/County Level Activities
 Mapping level tasks performed
at county level
 Nearshore wave transformations
 Wave runup
 Overland wave propagation
Response Based Analysis
 Attempt to consider all (or most) of the complexity of the
contributing processes controlling flooding and derive flood
statistics from the results
 Contributing processes to be considered:
 Water level
 Wave conditions
 Topography
Topography & Bathymetry
Updates to Guidance
D.3.1
D.3.2
Overview and Guidance
on Selection and
Application of Methods
(Instructions for Toolbox)
Detailed Guidance on
Analyzing Coastal Processes
Guidance on Use of Results in
Hazard Mapping,
Documentation, and
Reference Information
D.3.3
Waves and Water Levels
D.3.4
Wave Setup, Runup and
Overtopping
D.3.5
Overland Wave Propagation
D.3.6
Coastal Erosion
D.3.9
Study
Documentation
D.3.10
References, Notation,
and Acronyms
D.3.11 – D.3.13
Guidelines Overview and
Important Contributors to
Coastal Flooding
Methodology for Storm
Sampling and Coastal Flood
Frequency Analysis
Overview and Guidance
Application of Methods
(Instructions for Toolbox)
(Toolbox)
Guidance on Use of Results in
Hazard Mapping,
Documentation, and
Reference Information
Methodology for Analyzing
Coastal Processes
Mapping of Hazard
Zones and BFEs
Study
Documentation
Coastal Structures
D.3.8
D.3.7
Wave Setup
 Description of Wave Setup: localized impacts of water level at the
shoreline during severe storms due to transfer of momentum from
waves to the water column.
Wave Setup Implications for Flood Hazard
Mapping
 Can be a significant contributor to the water level through its
contribution to storm surge and should be included in the
determination of coastal BFEs.
 1-D Surf Zone Model
 Adequately resolve and represent inner surf zone
 Parametric representation
 Direct Integration Method
  2.0
0
'
0
2.0
'
0
_
160.0
LH
m
H

Wave Runup
Figure D.3.5-5. Wave Runup Sketch
Barrier Slope Breaker Depth
Limit of Wave Runup
Storm Still
Water Level
Source: FEMA, 2003
Wave Runup Approach
 Extract water level and wave pairings from the composite
storm set
 Apply a method to estimate wave runup for each of the
composite storm set pairings
 Conduct a statistical extreme value analysis on the runup
elevations to determine 1-percent-annual-chance
Wave Overtopping
 Overtopping Rate Considerations
for Establishing Flood Insurance
Rate Zones
 Ponding Considerations
Onshore Wave Analysis
Wave Runup Overland Wave Propagation
Overland Wave Propagation
 How waves interact with landforms
 Elevation
 Obstructions
 WHAFIS
 1977 NAS report
 Version 4.0
Transect
Hybrid Analysis
 WHAFIS is designed for event based analysis
 1-percent-annual-chance water level
 1-precent-annual-chance wave height
 Hybrid
 Joint probability approach (Nadal-Carabello et al, 2012)
 Water level
 Wave height
 Wave period
Five Scenarios
 Iso-probability curve
 Maximum water level, associated wave height
 Maximum wave height, associated water level
 Intermediate values
 Computed 1-percent-annual-chance water level
 Computed 1-percent-annual-chance wave height
Coastal Erosion
 Episodic, flood-related erosion due to coastal storm events
 Does not consider long-term erosion hazard areas
 Evaluated prior to wave runup and overland wave
propagation
Erosion Assessment Methods
 1-D surf zone dynamics model
 Requirements
 Cross-shore profile
 Sediment grain size
Coastal Structures
 Evaluation Criteria
 Detailed engineering evaluation (FEMA, 1990)
 Limited data and engineering judgment (USACE, 1989)
Vertical Structures
Sloped Structures
Updates to Guidance
D.3.1
D.3.2
Overview and Guidance
on Selection and
Application of Methods
(Instructions for Toolbox)
Detailed Guidance on
Analyzing Coastal Processes
Guidance on Use of Results in
Hazard Mapping,
Documentation, and
Reference Information
D.3.3
Waves and Water Levels
D.3.4
Wave Setup, Runup and
Overtopping
D.3.5
Overland Wave Propagation
D.3.6
Coastal Erosion
D.3.9
Study
Documentation
D.3.10
References, Notation,
and Acronyms
D.3.11 – D.3.13
Guidelines Overview and
Important Contributors to
Coastal Flooding
Methodology for Storm
Sampling and Coastal Flood
Frequency Analysis
Overview and Guidance
Application of Methods
(Instructions for Toolbox)
(Toolbox)
Guidance on Use of Results in
Hazard Mapping,
Documentation, and
Reference Information
Methodology for Analyzing
Coastal Processes
Mapping of Hazard
Zones and BFEs
Study
Documentation
Coastal Structures
D.3.8
D.3.7
Mapping a Coastal Floodplain
Mapping Example - Ortho
Mapping Example - Terrain
Mapping Example - Mapping Decisions
 Transect 11
 1% Total Water Level – 586.88 feet
 Top of coastal feature – 587.77 feet
 Base Flood Elevation – 587 feet
 Transect 12
 1% Total Water Level – 591.87 feet
 Top of coastal feature – 624.47 feet
 Base Flood Elevation – 592 feet
560
570
580
590
600
-100 100 300 500 700
Profile 1% Total Water Level/BFE
560
580
600
620
640
-100 0 100 200 300
Profile 1% Total Water Level/BFE
Mapping Example - Gutters
46
Brian Caufield, P.E., CFM caufieldba@cdmsmith.com
www.twitter.com/caufieldba

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History of Coastal Flood Hazard Assessments in Great Lakes

  • 1. June 23, 2016 The History of Coastal Flood Hazard Assessments in the Great Lakes Brian A. Caufield, P.E., CFM
  • 3. Some Statistics  Courtesy of Great Lakes Information Network  One-fifth of the world’s fresh surface water  Spread out over the contiguous U.S., would submerge the country under 9.5 feet of water  More the 94,000 square miles (larger than New York, New Jersey, Connecticut, Rhode Island, Massachusetts, Vermont, and New Hampshire combined)  10,900 miles of coastline (U.S. and Canada combined)  3,288 miles in Michigan (only Alaska has more) 3
  • 4. 4
  • 5. Just because an inland body of water doesn’t make it immune to risk  Fast moving squall lines can create localized risks  Passage of low pressure centers act similar to hurricanes  Central pressures recorded similar to those of a tropical or extra- tropical storm  Storms can create:  Surge  Waves 5
  • 7. Wave Runup Kennedy, Layne. 2010. September 4, 2014. http://laynekennedy.blogspot.com/2010_10_01_archive.html
  • 8. Overtopping Green, M. Spencer. AP Photo. 2012. September 4,2014. http://journalstar.com/ap/business/two-story-waves-on-great-lakes-halt-shipping/article_bcf2bb34-b528-52f5-8cd4-0c57e7ea8922.html
  • 9. Overtopping Jackson, Brian. North Ave. Beach. 2012. September 4, 2014. http://www.suntimes.com/photos/galleries/index.html?story=16046778
  • 10. Overland Wave Propagation Unknown. Flooding in Green Bay, WI. 1973. September 4, 2014. http://greatlakesresilience.org/stories/wisconsin/nor%E2%80%99easter-coastal-storm-flooding-green-bay
  • 11. Early attempts to identify flood risks 11
  • 12. Waves and Erosion  Waves  Leverage USACE Wave Information Study (WIS) 1956-1987  Local wave height with recurrence interval of 3 years approximately describes wave action likely to accompany the base flood  ½ year was used on Lake Ontario due to a different fit for the wave data on the lake  Erosion  Based on FEMA (1989)  Erosion (in square feet) = 85.6 * Recurrence Interval (in years)  270 square feet for 3-year recurrence  190 square feet for 2-year recurrence 12
  • 13. 2009 Update 1. Return period lake level recommended on a USACE (1988) report, but additional 20-years of observations 2. Wave runup is dominant risk and a response based approach is desirable 3. Previous wave guidance included long-term lake processes 13
  • 15. Combination of Water Levels and Waves 15
  • 16. Great Lakes Coastal Flood Study  Kicked off in 2009  Basin-wide assessment of flood risks  Updated Guidance 16
  • 19.
  • 20. Overall Process Offshore Waves Still Water Level Levels Wave Transformation If Necessary Flood Hazard Mapping Wave Height Wave Crest Elevation Wave Runup Wave Overtopping Erosion Shoaling Zone Surf Zone Backshore Zone Coastal Structures Wave Setup
  • 21. Study Approach  Regional Study Approach  Water level and wave analysis  Improvement over community- county  Reduces number of boundary conditions  Greater consistency in assumptions  Local/County Level Activities  Mapping level tasks performed at county level  Nearshore wave transformations  Wave runup  Overland wave propagation
  • 22. Response Based Analysis  Attempt to consider all (or most) of the complexity of the contributing processes controlling flooding and derive flood statistics from the results  Contributing processes to be considered:  Water level  Wave conditions  Topography
  • 24. Updates to Guidance D.3.1 D.3.2 Overview and Guidance on Selection and Application of Methods (Instructions for Toolbox) Detailed Guidance on Analyzing Coastal Processes Guidance on Use of Results in Hazard Mapping, Documentation, and Reference Information D.3.3 Waves and Water Levels D.3.4 Wave Setup, Runup and Overtopping D.3.5 Overland Wave Propagation D.3.6 Coastal Erosion D.3.9 Study Documentation D.3.10 References, Notation, and Acronyms D.3.11 – D.3.13 Guidelines Overview and Important Contributors to Coastal Flooding Methodology for Storm Sampling and Coastal Flood Frequency Analysis Overview and Guidance Application of Methods (Instructions for Toolbox) (Toolbox) Guidance on Use of Results in Hazard Mapping, Documentation, and Reference Information Methodology for Analyzing Coastal Processes Mapping of Hazard Zones and BFEs Study Documentation Coastal Structures D.3.8 D.3.7
  • 25. Wave Setup  Description of Wave Setup: localized impacts of water level at the shoreline during severe storms due to transfer of momentum from waves to the water column.
  • 26. Wave Setup Implications for Flood Hazard Mapping  Can be a significant contributor to the water level through its contribution to storm surge and should be included in the determination of coastal BFEs.  1-D Surf Zone Model  Adequately resolve and represent inner surf zone  Parametric representation  Direct Integration Method   2.0 0 ' 0 2.0 ' 0 _ 160.0 LH m H 
  • 27. Wave Runup Figure D.3.5-5. Wave Runup Sketch Barrier Slope Breaker Depth Limit of Wave Runup Storm Still Water Level Source: FEMA, 2003
  • 28. Wave Runup Approach  Extract water level and wave pairings from the composite storm set  Apply a method to estimate wave runup for each of the composite storm set pairings  Conduct a statistical extreme value analysis on the runup elevations to determine 1-percent-annual-chance
  • 29. Wave Overtopping  Overtopping Rate Considerations for Establishing Flood Insurance Rate Zones  Ponding Considerations
  • 30. Onshore Wave Analysis Wave Runup Overland Wave Propagation
  • 31. Overland Wave Propagation  How waves interact with landforms  Elevation  Obstructions  WHAFIS  1977 NAS report  Version 4.0
  • 33. Hybrid Analysis  WHAFIS is designed for event based analysis  1-percent-annual-chance water level  1-precent-annual-chance wave height  Hybrid  Joint probability approach (Nadal-Carabello et al, 2012)  Water level  Wave height  Wave period
  • 34. Five Scenarios  Iso-probability curve  Maximum water level, associated wave height  Maximum wave height, associated water level  Intermediate values  Computed 1-percent-annual-chance water level  Computed 1-percent-annual-chance wave height
  • 35. Coastal Erosion  Episodic, flood-related erosion due to coastal storm events  Does not consider long-term erosion hazard areas  Evaluated prior to wave runup and overland wave propagation
  • 36. Erosion Assessment Methods  1-D surf zone dynamics model  Requirements  Cross-shore profile  Sediment grain size
  • 37. Coastal Structures  Evaluation Criteria  Detailed engineering evaluation (FEMA, 1990)  Limited data and engineering judgment (USACE, 1989)
  • 40. Updates to Guidance D.3.1 D.3.2 Overview and Guidance on Selection and Application of Methods (Instructions for Toolbox) Detailed Guidance on Analyzing Coastal Processes Guidance on Use of Results in Hazard Mapping, Documentation, and Reference Information D.3.3 Waves and Water Levels D.3.4 Wave Setup, Runup and Overtopping D.3.5 Overland Wave Propagation D.3.6 Coastal Erosion D.3.9 Study Documentation D.3.10 References, Notation, and Acronyms D.3.11 – D.3.13 Guidelines Overview and Important Contributors to Coastal Flooding Methodology for Storm Sampling and Coastal Flood Frequency Analysis Overview and Guidance Application of Methods (Instructions for Toolbox) (Toolbox) Guidance on Use of Results in Hazard Mapping, Documentation, and Reference Information Methodology for Analyzing Coastal Processes Mapping of Hazard Zones and BFEs Study Documentation Coastal Structures D.3.8 D.3.7
  • 41. Mapping a Coastal Floodplain
  • 43. Mapping Example - Terrain
  • 44. Mapping Example - Mapping Decisions  Transect 11  1% Total Water Level – 586.88 feet  Top of coastal feature – 587.77 feet  Base Flood Elevation – 587 feet  Transect 12  1% Total Water Level – 591.87 feet  Top of coastal feature – 624.47 feet  Base Flood Elevation – 592 feet 560 570 580 590 600 -100 100 300 500 700 Profile 1% Total Water Level/BFE 560 580 600 620 640 -100 0 100 200 300 Profile 1% Total Water Level/BFE
  • 45. Mapping Example - Gutters
  • 46. 46 Brian Caufield, P.E., CFM caufieldba@cdmsmith.com www.twitter.com/caufieldba

Editor's Notes

  1. Recommend not saying “floodplain” but “high hazard area,” since geographically ,a floodplain is something totally different.