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Mapping the Zone: Improving Flood Map Accuracy. David Maidment, Chair Gerry Galloway. Briefing for FEMA January 15, 2009. Committee Charge: Task 3. 3. Investigate the impact that various study components (i.e., variables) have on the mapping of flood inundation boundaries:

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Mapping the zone improving flood map accuracy l.jpg

Mapping the Zone: Improving Flood Map Accuracy

David Maidment, Chair

Gerry Galloway

Briefing for FEMA

January 15, 2009


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Committee Charge: Task 3

3. Investigate the impact that various study components (i.e., variables) have on the mapping of flood inundation boundaries:

a. Riverine flooding

  • The accuracy of digital terrain information

  • Hydrologic uncertainties in determining the flood discharge

  • Hydraulic uncertainties in converting the discharge into a flood water surface elevation

    b. Coastal flooding

  • The accuracy of the digital terrain information

  • Uncertainties in the analysis of the coastal flood elevations

    c. Interconnected ponds (e.g., Florida)

  • The accuracy of the digital terrain information

  • Uncertainties in the analysis of flood elevations


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Committee Membership

Practitioners

Academics

Geodesy

Hydrology

Coastal

Economics

Risk

David Maidment, Chair, University of Texas

David Brookshire, University of New Mexico

J. William Brown, City of Greenville, South Carolina

John Dorman, State of North Carolina

Gerald Galloway, University of Maryland

Bisher Imam, University of California, Irvine

Wendy Lathrop, Cadastral Consulting

David Maune, Dewberry

Burrell Montz, Binghamton University

Spencer Rogers, North Carolina Sea Grant

Karen Schuckman, Pennsylvania State University

Y. Peter Sheng, University of Florida

Juan Valdes, University of Arizona


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Previous NRC Studies:Flood Map Technologies (2007)

  • An examination of the accuracy of flood base map input data

    • 2D imagery and planimetrics

    • 3D elevation

  • Prompted by issues raised by Senate Appropriations Committee staff


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Adjusted goal: 92% of population and 65% of land area will have a modernized map

21% of population has maps meeting the floodplain boundary standard and engineering study standard


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Flood Maps have a modernized map

Coastal

Riverine

Two very different flood modeling and mapping problems


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Riverine Flood Mapping have a modernized map

  • Modeling and mapping technology is well established

  • Supported by a large observation database at stream gages

  • Floods flow along the line of the stream gages


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Coastal Flood Mapping have a modernized map

  • Modeling and mapping technology and guidance are evolving

  • Storm surges inland transverse to the line of tide gages

  • Large dependence on models, less on historical flood data


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Terrain data accuracy matters have a modernized map

USGS NED (30m)

NCFMP Lidar (3m)

Inundation for a 1ft storm surge or sea level rise in the Tar-Pamlico estuary (Source: USGS)


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Lidar of inundated water surface elevation during Iowa flood (2008)

Source: University of Iowa and National

Center for Airborne Laser Mapping


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Three systems for measuring elevation (2008)

Orthometric heights

(land surveys, geoid)

Ellipsoidal heights

(lidar, GPS)

Tidal heights

(Sea water level)

Conversion among these height systems has some uncertainty


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Trends in Tide Levels (2008)(coastal flood risk is changing)

Charleston, SC

+ 1.08 ft/century

1900

2000

Galveston, TX

+ 2.13 ft/century

- 4.16 ft/century

1900

2000

Juneau, AK

1900

2000


Importance of geodetic datums navd88 ngvd29 cm l.jpg
Importance of geodetic datums (2008)NAVD88 – NGVD29 (cm)

NGVD29 higher in East

More than 1 meter difference

NAVD88 higher in West

Orthometric datum height shifts are significant relative to BFE accuracy, so standardization on NAVD88 is justified


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North Carolina Case Studies (2008)http://www.ncfloodmaps.com/program_review.htm

Economics

H&H

Studies done for the NRC Committee by the North Carolina Floodplain Mapping Program (NCFMP)

Mountains of Western NC

Rolling hills of Piedmont

Flat coastal plain

H&H and Economics

(H&H = Hydrology and Hydraulics)


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One River Reach studied in detail in each region (2008)(each reach 5-7 miles long)


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Terrain Data for Case Studies (2008)

USGS DEMs (30m)

NCFPM Lidar (3m)


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NED is higher (2008)

(green)

Lidar is higher

(purple)


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NED is higher (2008)

(green)

An elevation “bust”

Systematic and random errors


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Terrain Data (2008)

  • Our study demonstrates that there are large differences between LIDAR and NED

    • Random differences everywhere

    • Systematic differences in some places


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Defining Uncertainty in BFE (2008)Long term records of extreme stages recorded at USGS gages

At each gage the peak stage is recorded for each year along with the peak flow – do a frequency analysis of these.


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Frequency Analysis of Stage Heights at 31 gages (2008)

6

7

8

21 gages in NC

Is pitted FL landscape different?

All gages have at least 20 years record

(average is 54 years)

10 gages in FL


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Swannanoa River at Biltmore, NC (78 years of record) (2008)

Base flood discharge

Discharge (cfs)

T = 100 years

Annual Exceedence Probability

Produced using the Corps HEC-SSP Program (Bulletin 17-B standard procedure)


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Swannanoa River at Biltmore, NC (78 years of record) (2008)

95% CL

5% CL

Stage (ft)

Sampling error =

T = 100 years

Annual Exceedence Probability

Uncertainty in BFE = Uncertainty in 100-year stage height


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Sampling Error of 100-year Stage Heights (2008)

Outlier (skewed frequency curve)

No systematic variation in sampling error by

drainage area or topographic region

Sampling Error (ft)

Average = 1.06 ft

Drainage Area (Sq miles)


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BFE and Base Stage Height differ by a constant amount (gage datum – geodetic datum)

This doesn’t affect uncertainty of statistical variation of sample data around the 100-year estimate

Average value of sample error at 30 of 31 gage sites is 1.06 ft

A Lower Bound on the uncertainty of the BFE is a standard error of estimate of approximately one foot

Uncertainty in BFE

95% CL

5% CL

Base Stage Height

BFE, h

Gage datum

Geodetic datum


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Uncertainty in Floodplain Boundary Location datum – geodetic datum)

Lateral channel slope is calculated on HEC-RAS cross-sections at the point of intersection of water surface with land surface (left and right banks) and averaged for all cross-sections in the reach

dw/dh = Run/Rise

w

dh

h

dw

A Lower Bound on the uncertainty of the floodplain boundary location ranges from approximately 8ft in the mountains to approximately 40 ft in the coastal plain


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Hydrologic and Hydraulic Methods datum – geodetic datum)

100-yr Discharge

Base Flood Elevation

Floodplain Map

Mapping

Hydraulics

Hydrology


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USGS datum – geodetic datum)Peak-FlowRegression Equationsfor 100-year discharge


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Age of Rural Peak Flow Regression Equations datum – geodetic datum)

Some equations are old

Need for equations to follow basin rather than state boundaries


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Effect on BFE of Variation in Hydrologic Methods datum – geodetic datum)(Long Creek, Mecklenburg County)


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Effect of Hydrologic methods on BFE datum – geodetic datum)

  • Choice of hydrologic method affects the BFE by usually less than 1 foot

  • All methods in our study are calibrated to the gage frequency curve and all our reaches have a gage, so gage calibration dominates variation in hydrologic methods

  • Stream gage data are important


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Hydraulic Model Uncertainties datum – geodetic datum)


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Case Study: Hydraulic Model-Terrain Variants datum – geodetic datum)

Detailed

Limited Detailed

Approximate

(lidar)




Effect on bfe of variation in hydraulic methods and terrain data long creek l.jpg
Effect on BFE of variation in hydraulic methods and terrain data (Long Creek)

Approximate Study using NED

21 ft


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Approximate Study BFE Profiles data (Long Creek)

Approximate - Lidar

Approximate - NED

Misalignment (100 – 200 ft) of mapped 2D planimetric streamline with NED 3D elevation data


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Flood Hazard Zone Areas data (Long Creek)

Swannanoa River

  • At Ahoskie Creek and Swannanoa River the number of acres enclosed in the SFHA by Detailed and Approximate studies differs by < 1%

  • Difference at Long Creek = 20%

Detailed - lidar

Detailed - NED

Approximate-NED

Approximate studies give the same area of flood zone but a different shape


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Interconnected Ponds (e.g. Florida) data (Long Creek)

  • Gage study showed that BFE uncertainty in Florida rivers is similar to NC

  • Many complex hydrologic issues inherent in how water reaches river from a ponded landscape

  • Needs a separate study

Data from SWFWMD


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Overarching Finding data (Long Creek)

1. Topographic data is the most important factor in determining water surface elevations, base flood elevation, and the extent of flooding, and thus the accuracy of flood maps in riverine areas


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Coastal Flood Mapping data (Long Creek)



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Risk and Floodplain Mapping data (Long Creek)


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Risk data (Long Creek)

The probability of an event multiplied by the consequences if the event occurs

Risk = p x c

Risk = p x cn

p = probability (h, s)

c = consequences

n = variable related to

social values

p = probability (hazard, system)

c = consequences


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Risk Maps data (Long Creek)


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Conclusions data (Long Creek)

  • Riverine

    • Elevation, elevation, elevation

  • Coastal

    • Inundation process is complex

  • Economics

    • Base flood elevations are worth it

  • Risk

    • Better maps can provide good risk information


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