Substrate mapping

Thematic maps of tidal and near-shore terrestrial areas provide a basis for coastal zone sensitivity assessment and for other applications such as military reconnaissance mapping. Imagery in a single polarization is generally inadequate for discriminating coastal zone features. Multi-polarization or polarimetric imagery can be used to effectively discriminate the structural differences of various coastal features. Figure 9.46 shows an inter-tidal flat in the Minas Basin of the Bay of Fundy. The tidal flat is gently sloping (1 to 2°) and consists of friable sandstone, mudflats and gravel and boulder deposits along the channel. In the multi-polarization colour composite, regions corresponding to various substrates can be separately identified. The green tone associated with the area of sandstone indicates the dominance of the cross-polarized return that is typically associated with volume or multiple scattering. The mud flats show a very low backscatter return in images in the HH and HV polarizations, while the gravel and boulder deposits (white) are indicative of high backscatter return seen in imagery at all three of the polarizations.

Polarimetric signatures for regions of different substrates within the tidal zone are shown in Figure 9-47. Each signature shows that backscatter is maximal at the VV polarization The mud flats exhibit a very low pedestal height (0.03), and the higher pedestal heights for sandstone and gravel suggest an increase of the unpolarized component due to rough surface scattering. A more prominent backscatter return in the HH polarization is evident in the area of the gravel/boulder substrate indicating significant double bounce scattering.

9.6.2.1 Polarimetric Classification

Did you Know?


The type of substrate along a coastline is important for environmental reasons such as susceptibility to erosion, oil spill remediation and habitat evaluation, as well as for military applications such as suitability as a landing site with respect to trafficability.

Polarimetric classification according to scattering mechanism may provide additional useful information regarding target characteristics within tidal zones. Figure 9-48 shows a simple classification of the tidal flat using the method outlined by van Zyl (1989). It classifies the dominant scattering behaviour of each pixel into one of three scattering classes: Odd Bounce scattering, Even Bounce scattering, or diffuse scattering.

A = Sandstone  B = Mud  C = Gravel
Red = Even (double)
Green = Diffuse
Blue = Odd

The classification results show that mud flats within the tidal zone are predominantly surface scatterers (Odd Bounce) characteristic of a smooth to slightly rough surface, sandstone areas are predominantly characterized by Odd Bounce scattering with a mix of Even Bounce and diffuse scattering. The gravel areas tend to have a high portion of Even Bounce scattering due to the presence of small boulders that act as corner reflectors.

Whiz quiz

Question: Why is imagery in the cross polarization better than that in VV for identifying the land/water boundary? The answer is...

Whiz quiz - answer

Answer: Water is a surface scattering target with a very low backscatter at HV compared to land thus resulting in better land-water contrast. Also the VV polarization is more sensitive to wind induced surface roughness resulting in lower contrast between land and water.