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Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil, Architectural, and Environmental Engineering University of Texas at Austin 1

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Page 1: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

Hydrodynamic modeling for river delta salt marshes using lidar

topographyA Cell-Edge technique for bathymetric processing

Ben R. HodgesDept. of Civil, Architectural, and Environmental

EngineeringUniversity of Texas at Austin

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Page 2: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

The lidar challenge for hydrodynamics

• Processed lidar at 1x1 m resolution• Hydrodynamic models at 10x10 m or coarser.• Simple averaging loses information.• Ho do you handle subgrid data?• Today we’ll look at an example of

topographical processing for hydrodynamic representation.

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Page 3: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

Where we are working...

Texas coastimage from Google Earth

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Page 4: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

Where we are working...

Corpus Christi

Houston

image from Google Earth

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Page 5: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

Where we are working...

Nueces River Delta

City of Corpus Christi

image from Google Earth

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Page 6: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

Nueces River Delta

image from Google Earth

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Page 7: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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1 x 1 m ~ 120 x 106

10 x 10 m ~ 1.2 x 106

30 x 30 m ~ 130,000

data processed by J. Gibeaut, Texas A&M Corpus Christi

Page 8: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 9: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 10: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 11: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 12: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 13: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 14: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 15: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 16: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

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Page 17: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

Summary of Cell-Edge technique

• Use median filter on fine grid data with Matlab medfilt2() function for baseline coarse grid.

• Identify coarse grid cells with a large fraction (45%) of subgrid cells that are a defined increment (0.2 m) higher than coarse grid median and use 75th percentile for coarse grid elevation.

• In each coarse grid cell, begin at median elevation and sweep upwards in elevation increments (0.1 m) using Matlab bwboundaries() function to identify obstacles.

• Find highest obstacle that crosses entire cell on X axis, and create an edge feature in X direction.

• Repeat for Y direction.

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Page 18: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

Conclusions• Image processing techniques (available in Matlab) provide

powerful tools for bathymetric processing.• Advantage of Cell-Edge method: Creates a coarse grid array

with cells and edges that create hydraulically blocking features.

• Open issue: How to confirm that the edges are continuous?• Open issue: 75th percentile elevations on high cells tend to

slightly underestimate blocking elevation.• Open issue: How to handle connectivity of subgrid channels?• Disadvantage: Median filter is computationally expensive for

large arrays.

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Page 19: Hydrodynamic modeling for river delta salt marshes using lidar topography A Cell-Edge technique for bathymetric processing Ben R. Hodges Dept. of Civil,

Acknowledgements• Coastal Bend Bays and Estuaries Program• U.S. National Science Foundation• Texas Water Development Board• City of Corpus Christi• U.S. Army Corps of Engineers

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