2.5 - Bidirectional reflection

So far we have seen that the visual perception of colour is related to the differential absorption/reflection of radiation by an object in the different regions of the electromagnetic spectrum. But why do we perceive different intensities of light? What physical explanation is behind the creation of patterns of lightness and darkness?

To answer to this question we must consider the different ways an object may reflect light. This is primarily a function of the object surface's roughness.

EXERCISE LOST DUE TO FLASH DISCONTINUATION

The Sun Glint effect mentioned in the exercise can be seen in following figure

Figure 2.11: Sun glint over the east Mediterranean on 8 May 2016 at 07:49 UTC

2.5.1 - BRFDs

The measured surface reflectance depends on the configuration: sun position - observation geometry.

First think of a geostationary satellite, located at fixed position above the Earth. For each individual pixel only the Sun geometry varies from slot to slot.

For the case of polar orbiters, (normally sun-synchronous) it is mainly the satellite observation angles that change between observation slots of the same region.

This means that reflectance values measured with geostationary or polar satellites need to be corrected for directional effects. Such corrections may be easily performed if the Bidirectional Reflectance Distribution Functions (BRDF) are known. The BRDF model describes reflection behavior for all possible combinations of sun-viewing geometries. The characteristics of the BRDF will determine what "type" of material the viewer thinks the displayed object is composed of.

Among the several Bi-directional Reflectance Distribution Functions proposed by different authors, the one by Roujean et al. (1992) has been extensively used for vegetation parameters estimations:

ρ (θs, θv, φ) = K0 + K1 x F1(θs, θv, φ) + K2 x F2(θs, θv, φ)

F1 and F2 are functions, called kernels, which only depend on the angular configuration of aquisition:

  • θs is the sun zenith angle;
  • θv is the satellite zenith angle
  • φ is the relative azimuth angle between sun and satellite

The K coefficients quantify the respective contribution of each kernel to the whole BRDF and are derived by model inversion.

  • K0 corresponds to isotropic reflectance, i.e. reflectance values directionally normalised to reference illumination and observation zenith angles of 0°. This geometry leads to a minimum of the shadow proportion (hotspot geometry);
  • K1 and K2 represent angular distribution related to geometric (caused by diffuse reflectors) and volumetric (caused by volume scatter reflectors) surface scattering processes.

The isotropic, geometric and volumetric components of surface reflectance are intrinsically linked to the amount and state of vegetation, canopy structure and to the leaf and soil optical properties, as you will see in more detail in chapter 5.