Siddhi Joshi
MSc Hydrographic Surveying
UCL
Research into the Use of Multibeam Backscatter for
Seabed Classification in the Outer Thames Estuary
Abstract
Multibeam systems collect both bathymetry and backscatter data
and can be used for seabed classification. Two different approaches
to seabed classification, the image-based method and the angular
response characterisation approach have been studied
andsubsequently compared. Seabed classification methods are one way
of characterising theseabed and have many applications in the field
of seabed mapping. This study has used the Quester Tangent
Corporation (QTC) image-based method and the newer
Geocodersoftware's angular response characterisation approach to
characterise two areas affected by dredging activities. The QTC
approach divides the region into discrete classes, which are
subsequently identified by groundtruthing. Geocoder is able to make
remote estimates of the physical properties of the seafloor using
the Angular Range Analysis (ARA) method.
First, the North Edinburgh Channel sand placement site,
monitored by the Port of London Authority, is studied. Results
include different types of multibeam backscatter mosaics, partially
stacked backscatter, angular response curves and remote estimates
of the grain size. Overall, Geocoder results here show good
agreement with groundtruthing. The QTC unsupervised classification
approach is used to identify and monitor the classes in the area of
relocation. This effectively distinguishes between the coarser
relocated material and classes in the North Edinburgh Channel
seabed.
Geocoder ARA results from the second site; the Thames Regional
Environmental Characterisation survey area, has been studied and
compared with the QTC classification. Results suggest that the QTC
method can more effectively discriminate between areas affected by
aggregate extraction in this region. The Geocoder software however
shows great potential, allowing quantitative information about the
grain size, acoustic impedance and seafloor roughness to be
determined using multibeam data. Both approaches have their merits
and can be used as part of seabed characterisation studies in a
wide range of applications.