APPLICATION OF LIDAR IN FLOODPLAIN MAPPING - PowerPoint PPT Presentation

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APPLICATION OF LIDAR IN FLOODPLAIN MAPPING

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GIS and hydraulic models to map the possible extent of flooding, and to prove ... Softwares used : ArcGis ( Arctoolbox, ArcMap),Arcview , HEC-RAS HecGeoRas extension ... – PowerPoint PPT presentation

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Title: APPLICATION OF LIDAR IN FLOODPLAIN MAPPING


1
APPLICATION OF LIDAR IN FLOODPLAIN MAPPING
Imane MRINI GIS in Water Resources University of
Texas at Austin
Source. Optech,Inc
2
PURPOSE OF THIS PROJECT
  • Show how LIDAR technology can be used jointly
    with
  • GIS and hydraulic models to map the possible
    extent of flooding, and to prove that it could be
    an invaluable tool in flood mapping because of
    its high accuracy.

3
WHAT IS LIDAR ?
Acronym for Light Detection And Ranging
  • Airborne laser system used to acquire x, y, and z
    coordinates of terrain, and consist of
  • Airborne Global Positioning System (GPS)
  • Attendant GPS base station
  • Inertial Measuring Unit (IMU)
  • Light-emitting scanning laser.

4
HOW LIDAR WORKS
  • Laser pulse rate up to 25,000 per sec.
  • Operating altitude 400 - 2,000 meters.
  • Swath width up to 1,500 meters
  • at 2,000 meter altitude.

5
PRECISION OF THE LIDAR DEM
Source.BEG
6
LIDAR INSTRUMENT All-Terrain Laser Mapper (ALTM)
7
LIDAR FACTS
  • Elevation accuracy 10 to 25 cm
  • records first and last returns of individual
    pulses and intensity

Applications in ? Flood mapping ? Forest
management ? Coastal management ? Land cover
classification ? Atmospheric pollution monitoring
8
DATA PROCESSING Source BEG
  • compute a differentially corrected aircraft
    trajectory using a GPS software,
  • generate the raw x, y, and z data,
  • grid the data to generate an all-points DEM,

(4) filter the raw data and re-grid to generate a
vegetation-removed DEM
9
EFFECT OF VEGETATION REMOVAL
After
Before
10
FLOODPLAIN MODELING
  • Study area Waller creek watershed in Austin,TX
  • LIDAR data source Bureau of Economic Geology-
    University of Texas at Austin
  • Type of Lidar data 1m DEMs of the all-point and
    bare-earth data as interchange files ( e.00)
  • Spatial reference UTM zone 14, datum NAD 1983
  • Softwares used ArcGis ( Arctoolbox,
    ArcMap),Arcview , HEC-RASHecGeoRas extension

11
STUDY AREA
Waller Creek Watershed
12
ALL-POINT LIDAR DATA OF WALLER CREEK
13
BARE EARTH LIDAR DATA FOR WALLER CREEK
14
FLOOD MODELING PROCEDURE
HEC-GeoRas Preprocessing
Geometric data stream centerlines, riverbanks,
floodplain boundaries, cross-sections along the
streams
ARCVIEW Terrain model processing
Hydraulic modeling
Flood map visualization
HEC-GeoRas Postprocessing
Import file
LIDAR input data 1m grid DEM
Hydrologic modeling
Plan data ( Flow regime)
Flow data from HEC-HMS
15
Extracting geometric data
  • Use of Spatial Analyst ,3D Analyst and
    Hec-GeoRas extensions
  • Using HEC-GeoRas extension and the digitizing
    tool in Arcview, I generated
  • - Streamcenterlines
  • - Stream banks
  • - Flow path centerlines
  • - Cross section lines

16
STREAM CENTERLINES
17
STREAM BANKS
18
FLOW PATH LINES
19
CROSS-SECTIONS CUTLINES
20
DIFFICULTY ENCOUNTERED
  • Problem Hec-GeoRas program only works with TINs
  • Solution Convert grids to TINs in ArcMap using
    the best vertical accuracy to generate the
    maximum number of triangles in a reasonable
    amount of time

21
CONVERTING TINs TO GRID
22
EXTRACTED CROSS SECTIONS
23
PREPARING THE IMPORT FILE TO HEC-RAS
24
DIFFICULTY ENCOUNTERED AT THIS STAGE
  • An error message from the Hec-PreRAS program
    during the import file process.

25
WORK TO BE DONE MODELING WITH HEC-RAS
  • Cross-section extracted
  • from the TIN.
  • RAS stream geometry.
  • Resulting water
  • elevations.

26
PREVIOUS FLOOD MAPPING WITH TINs (Source. Esteban
Azagra)
27
Future work
  • Solving the problem of the HecRas import file,
    hopefully before December 6
  • Potential ideas to develop
  • - Write a program that incorporate grid data in
    the preprocessing for HEC-RAS
  • Obtain a more detailed TINs from the grid
    conversion

28
ACKNOWLEDGMENT
  • Dr. David Maidment, University of texas at Austin
  • Becky Smith, Bureau of Economic Geology,
    University of Texas at Austin
  • John Andrews, Bureau of Economic Geology,
    University of Texas at Austin
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