RIEGL Bathymetry Hard- and Software Solutions. Andrea Spitzer, MASc Application Engineer

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RIEGL Bathymetry Hard- and Software Solutions Andrea Spitzer, MASc Application Engineer aspitzer@riegl.com May 27th, 2014

AGENDA» RIEGL VQ-820-G topo-bathy laser scanner» product specifications» results» software add-ons for hydrography» clutter filtering» point classification» water surface modeling» refraction correction

laser scanner for combined topographic and bathymetric applications

RIEGL VQ-820-G concept combined hydrographic and topographic laser scanner with narrow laser beam high range resolution high measurement rate compact and lightweight design dedicated for high-resolution mapping of shallow waters with low turbidity

VQ-820-G product specifications wavelength measurment range topography water penetration ranging accuracy 532 nm (visible green light) 1500 m at ρ 20% 2500 m at ρ 60% 1 Secchi depth bright ground 25 mm FOV 42 beam divergence measurement rate scan speed laser Safety multiple time around 1 mrad up to 195 khz 50 200 lines/s laser class 3B yes, up to 4 pulses in the air

VQ-820-G features excellently suited for combined land and hydrographic airborne survey high-accuracy ranging based on echo digitization and online waveform processing with multiple target capability high spatial resolution due to laser repetition rate up to 520 khz, high scanning speed up to 200 scanlines/second and a wide field of view 42 compact, rugged and light-weight modular configuration, compatible with standard airborne platforms. optional waveform data output, data accessible via RiWAVELiB seamless integration with other RIEGL ALS Systems and software packages

RIEGL echo waveform point cloud profile exemplary waveform water surface echo distributed reflection from turbid water body ground echo

RIEGL s complete system solution VQ-820-G DR-680 (optional) various topo-infrared laser scanners (optional) complete software solution

different ways of using RIEGL ALB systems

VQ-820-G integrated in a helicopter

VQ-820-G integrated in a Tecnam P2006T

VQ-820-G integrated in a CASA 212

ship-borne integration of VQ-820-G hydro-archeological survey pile dwellings at the Lake Constance

VQ-820-G integrated in a UAV Schiebel Camcopter

Baltic sea, Atlantic floodplains, rivers

floodplains example project floodplain near the Danube / Austria

floodplains example data - analyzed waterbody waterbody 250 m x 50 m x 4 m partly covered with ice surrounded by mixed vegetation powerlines 2,500 measurements from surface 400,000 subaqueous points

floodplains example data - surveying area partly covered with ice

floodplains example data - surveying area partly covered with ice

floodplains example data - results cross-section of the detailed topo-bathy point cloud data acquired in a single fly-by

costal survey example data surf zone and beach near Rostock/Germany

sand banks in 4m depth high point density on small structures

measurement from eyesafe hight broad flight strip from 600 m AGL still satisfactory penetration

Fjord Mapping near Stavanger from ~1000m cliffs down to ~10m below sea surface within one flight by

Ft. Lauderdale test project together with NOAA

Ft. Lauderdale example of the results zone with lots of seaweeds / very dark sediment

Ft. Lauderdale example of the results

Florida Keys example of the results

Adriatic Sea - example data

Adriatic Sea - example data more than 15 m depth from eye-safe altitude

large-scale surveying of rivers full coverage of riverbed, riverbank, and surrounding area requires careful planning concerning precipitation, snowmelt etc.

river mouth of Lake Ammersee, Estuary

Isar, Midsize river

Isar, Midsize river

point cloud classification refraction correction

what it s all about Post-processing of bathymetric LiDAR data is different to topographic LiDAR data. Additional correction due to different medium (air / water) is needed. Change in direction length

detection of isolated points analysis based on number of neighboring points

classification of water surface points - fully automatic approach - each scan line (strip) is processed independently - input: geo-referenced scan line with sufficient quality

classification of water surface points outline of method (1) 1.) find MLW cells by analyzing point distribution cell by cell - Most Likely Water cell - contains two well-separable point sets (in z-coordinate direction) - upper layer is supposed to contain water surface points - determine z-offset of cell s upper layer w.r.t. reference surface

classification of water surface points outline of method (3) 4.) growth algorithm to find further potential water cells starting from MLW cells 5.) examine potential water cells for water surface points

classification of water surface points examples white caps high waves motor boat typical profiles crossing coast line

classification of water surface points examples (2) Aerial image water surface (left) vs. low vegetation (right)

generation of a water surface model (WSM) - generated for each scan (strip) based on classified water surface points - WSM is represented by grid model (GRCS) aligned to main flight direction - WSM cell information: height (z GRCS ) and normal vector

generation of WSM outline of the method step 1: consider only cells with sufficiently high point density - if cell information meets criteria for cell type 1 - store WSM parameters - otherwise: cell type 2 or cell type 3

generation of WSM extrapolation ocean step 2: derive extrapolated WSM for remaining cells mode ocean assumption: water surface is more or less at the same level (cell of type 1)

generation of WSM extrapolation river step 2: derive extrapolated WSM for remaining cells mode river Due to slope: use individual z-offsets instead of a global one. Note: extrapolation is only done within buffer zone around water surface points

generation of WSM complete the model step 3: Complete the WSM smoothen extrapolated WSM at transitions to type-1 cells

generation of WSM results (1) WSM in case of high waves (ocean mode): elevation WSM (displayed as normal vector field) and water surface points (z-color-coded)

generation of WSM results (2) WSM (river mode): WSM (displayed as normal vector field) and water surface points (z-color-coded) note: WSM is only available in vicinity of water surface points; elsewhere: no-data values

refraction correction (1) Intersection of ray with WSM:

refraction correction (2)

conclusion RIEGL VQ-820-G topo-bathy laser scanner successfully employed for a great variety of applications quality of water surface model is essential for quality of bathypointcloud RIEGL provides a fully-automated turnkey solution for point classification and refraction correction RIEGL software workflow offers interfaces for custom-specific point classification or WSM

RIEGL Laser Measurement Systems GmbH Riedenburgstraße 48 3580 Horn, Austria Phone +43 2982 4211 office@riegl.com