3.2. Neumann Decomposition
In a fully polarimetric SAR system, the acquired scattering matrix in H-V polarization basis can be expressed as [
4,
5]
where
(
) represents the scattering coefficient from transmitting with
polarization and receiving with
polarization. After assuming the reciprocal scattering (i.e.,
), the corresponding Pauli-basis vector can be expressed as [
4,
5]
Then, the corresponding coherency matrix is given as [
4,
5]
Some years ago, Neumann proposed a model-based incoherent PolSAR decomposition method whose key contribution is the introduction of a generalized volume scattering model, which is defined by two parameters: the particle shape and the orientation randomness [
37,
38,
39]. Similar to the basic principle of the volume scattering modelling in Freeman–Durden or Yamaguchi-based methods, the Neumann volume scattering model is based on assuming the volume as a cloud of randomly oriented particles, and the orientation angle follows a certain statistic distribution. The normalized coherency matrix for one scattering particle in the volume is defined as [
37,
38,
39]
where
is the particle scattering anisotropy, of which the magnitude indicates the effective shape of an average particle. In general, when
is close to zero, the effective shape tends toward an isotropic sphere/disk. As
approaches one, the effective shape is close to a dipole (i.e., thin cylinder). The sign of real part of
determines the tendency of the particle axis of symmetry. It tends to be horizontal for
and vertical for
. The phase of
, i.e.,
, is more related to the orientation direction of the particles. From the mathematic point of view, it can be seen that
is related to the sign of real part of
. For
, the particles tends to be horizontal (
) and vertical (
) for
. In Freeman–Durden or Yamaguchi-based methods [
23,
24,
25,
26,
27], the scattering particle is one specific case, which assumes the scatterer is horizontal or vertical dipole, i.e.,
. Since the tendency somehow represents the morphological structure information, obviously it depends on the vegetation type. Theoretically,
or
can be used to help distinguishing the land cover types. However, from the perspective of independence of random variables, the magnitude and phase of
(i.e.,
and
) are selected as classification features in this study.
Assuming the particle is rotated by an angle
around the radar line of sight (Los), the coherency matrix describing a cloud of volume particles can be obtained by the integration of coherence matrix of a single particle over the orientation angles.
where
is the rotation matrix and
is the probability distribution function of orientations of the volume scatterers. Under the central limit theorem condition, Neumann suggests the orientation angle of volume scatterers follows a von Mises distribution (also known as the circular normal distribution), which can be expressed as [
37,
38,
39]
where
represents the degree of concentration,
is the mean orientation angle, and
denotes the modified Bessel function of order zero. For a simple geometrical interpretation, the normalized degree of orientation randomness
is defined as [
37,
38,
39]
With the variation of
, the volume can change from a preferred orientation direction (
) to completely random (
). Under the linear approximation for the orientation distribution, one can obtain two linear models for the coherency matrix form [
33,
37,
38,
39]
where the sum of diagonal elements is one. From Equation (8), it can be seen that Neumann generalized volume scattering model depends on two morphological vegetation parameters:
and
. As it was analyzed in [
37,
38], the Neumann general vegetation model agrees with some typical models. When
is equal to one, i.e., completely random case, it is the same as the volume scattering model in Freeman two-component decomposition. Two Yamaguchi volume scattering models are also approximately considered as two special cases of it [
37,
38].
It should be noted that Neumann generalized volume scattering model could be incorporated in any PolSAR/PolInSAR model-based decomposition framework [
33]. However, the Neumann decomposition is generally employed by matching completely the Neumann volume scattering model to the observed coherency matrix in order to directly invert two model parameters. In this case, the parameters from Neumann decomposition are defined as [
37,
38,
39]
Then, the particle scattering anisotropy magnitude and phase (i.e.,
and
), and the orientation randomness τ are adopted in this work as three polarimetric features for crop classification. In addition, in order to reduce the effects of overestimation of cross-scattering due to some uncertain reasons, such as topography slopes, it is usual to carry out the polarimetric orientation angle (POA) compensation (also called deorientation processing) proposed by Lee et al. [
41] before the Neumann decomposition.
It can be proven that these parameters are related to other existing scattering models and scattering mechanism types. In [
37,
38,
39], Neumann found that two of polarimetric feature parameters derived from Neumann decomposition have close relationships with the classical and commonly used Cloude–Pottier decomposition. The basic idea of Cloude–Pottier (CP) decomposition is to express the observed coherency matrix as a sum of three independent targets according to eigenvector and eigenvalue analysis. Then, this decomposition can be described as [
4,
5,
34]
where
,
and
are three eigenvalues of coherency matrix and
. The corresponding three eigenvectors are
,
and
. Then, the polarimetric scattering entropy
, averaged alpha angle
and polarimetric anisotropy
are defined as [
4,
5,
34]
where
can be determined by the eigenvectors because
is same as the magnitude of the first component of the eigenvector
. The polarimetric scattering entropy
indicates the scattering randomness degree. It ranges from 0 to 1, which represents from specifically identifiable scattering or deterministic scattering to complete random scattering. The value of angle
represents the scattering mechanism types in the scattering medium, which ranges from 0 (surface scattering) to 90° (double-bounce scattering). In particular, as it reaches the medium value of 45°, it represents dipole scattering or linearly-polarized scattering by a cloud of anisotropic particles [
4,
34]. The polarimetric anisotropy
ranges from 0 to 1, which measures the relative importance between the secondary scattering mechanisms. It should be noted that
becomes a very useful parameter to help to distinguish different scattering types only for medium values of
H [
4,
34]. In this case, the secondary scattering mechanisms play an important role in the scattering process.
Afterward, Neumann found the particle scattering anisotropy magnitude
to be directly related to the
angle in CP decomposition, i.e., [
37,
38,
39,
40]
The parameter |
δ| either represents the shape of the particle, if volumetric particle scattering is assumed, or the scattering mechanism type, if a mixed scattering mechanism is assumed. In theory, the range of |
δ| is assumed to be restricted within [0,1] under the Born approximation for a cloud of simple spheroidal particles. As it is an indicator for multiple scattering effects in the canopy, which are neglected by the Born approximation, the value of |
δ| could be larger than 1 [
39]. The general relationship between
and
is shown in
Table 3.
From the definition of orientation randomness
in Neumann decomposition and polarimetric scattering entropy
in Cloude–Pottier decomposition, it is easy to understand that both parameters describe the scattering randomness in the scattering medium.
Figure 4 shows the dependence of polarimetric scattering entropy
on the orientation randomness
with different value of the particle scattering anisotropy magnitude. It can be seen that generally the values of polarimetric scattering entropy
will monotonically rise with an increase of orientation randomness
. In particular, the values of orientation randomness become meaningless for
because the effective particle shape is considered as the isotropic scatterer in that case. Moreover, as the effective particle shape varies from isotropic scatterer (
) to dipole scatterer (
), the degree of scattering randomness in the medium increases gradually.
From the analysis mentioned above, it is clear that the two parameters (, ) derived from Neumann decomposition have significant correlation with the two parameters (, ) derived from Cloude–Pottier decomposition. In addition, the third parameter ( or ) in Neumann decomposition or Cloude–Pottier decomposition can also enhance the ability in distinguishing land cover types. The parameters derived from Cloude–Pottier decomposition are frequently used in land cover classification studies. In this regard, Neumann decomposition parameters should have the potential for land cover classification.