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MARINE SCENARIO - WAVE FRONT DETECTION
Touria BajjoukiFremer, France
IQmulus, Final WorkshopBergen, September 21, 2016
The research leading to these results has received funding from the European Union Seventh Framework Programme (FP7/2007-2013) under grant agreement n° 318787.
IQmulus workshop, Bergen
LIDAR WAVEFORM - MOTIVATION
o Airborne Lidar is a widely adopted technology for shallow coastal waters applications, o Contains much more information (useful for end-users) than simple bathymetry,o There is no commercial tool to handle this complex data.
Production of a seafloor 2D map with labels corresponding to identified sea bottom typesUsing Bathymetric Lidar Full WaveForm Data
I Q M U L U S U S E R S T O R I E S : 3 9 T O 4 3
U S E R E X P E C TAT I O N S
Allows to o extract from the lidar waveform parameters (Peak height, Pulse width, Pulse area, …) useful for classification of Seabed bottom types.
S E R V I C E 11 2 - B W F 2 _ W F _ AT T R I B U T E _ E X T R A C T I O N
S E R V I C E 111 – B W F 1 _ W F _ I N D E X I N GPerforms both sequential and spatial indexing
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IQmulus workshop, Bergen
Hard Substrate
Classification Soft Substrate
Vegetation
28 Waveform Attributes
MS5 WORKFLOW
(Octave)
21/09/2016
IQmulus workshop, Bergen
QUALITY-BIG DATA ASPECT
Roches de Penmarc’hMolène Archipelago
H AW K E Y E I I U S E D D ATA
Brittany RegionField data showing the presence (green) and absence (brown) of vegetation overlayed on Pulse Area
o Tested on several small and larger scale survey data sets from the Hawk Eye II system o Compared to ground truth data (video and diving samples) on sea bottom types
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