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Technical Note

A New Probability Distribution for SAR Image Modeling

1
Programa de Pós-Graduação em Engenharia de Produção, Universidade Federal de Santa Maria, Santa Maria 97105-900, Brazil
2
Departamento de Estatística, Universidade Federal de Santa Maria, Santa Maria 97105-900, Brazil
3
Departamento de Estatística and LACESM, Universidade Federal de Santa Maria, Santa Maria 97105-900, Brazil
4
Department of Telecommunications, Aeronautics Institute of Technology (ITA), São José dos Campos 12228-900, Brazil
*
Author to whom correspondence should be addressed.
These authors contributed equally to this work.
Remote Sens. 2022, 14(12), 2853; https://doi.org/10.3390/rs14122853
Submission received: 6 May 2022 / Revised: 26 May 2022 / Accepted: 6 June 2022 / Published: 14 June 2022

Abstract

:
This article introduces exponentiated transmuted-inverted beta (ET-IB) distribution, supported by a continuous positive real line, as a synthetic aperture radar (SAR) imagery descriptor. It is an extension of the inverted beta distribution, an important texture model for SAR imagery. The considered distribution extension approach increases the flexibility of the baseline distribution, and is a new probabilistic model useful in SAR image applications. Besides introducing the new model, the maximum likelihood method is discussed for parameter estimation. Numerical experiments are performed to validate the use of the ET-IB distribution as a SAR amplitude image descriptor. Finally, three measured SAR images referring to forest, ocean, and urban regions are considered, and the performance of the proposed distribution is compared to distributions usually considered in this field. The proposed distribution outperforms the competitor models for modeling SAR images in terms of some selected goodness-of-fit measures. The results show that the ET-IB distribution is suitable as a SAR descriptor and can be used to develop image-processing tools in remote sensing applications.

1. Introduction

Statistical modeling provides technical support for synthetic aperture radar (SAR) image processing and interpretation, allowing a better understanding of the terrain scattering mechanism [1]. It is also a recurring topic in radar-signal-processing applications such as edge detection [2], land cover classification [3], and target detection [4].
Depending on the SAR system characteristics, such as bandwidth, central frequency, pulse format, number of looks for generating the final image, and scene under observation, certain distributions can be more suitable for modeling it [1]. The Rayleigh and Weibull distributions are commonly used for modeling amplitude in single-look SAR images [1], and the exponential and Weibull are typical choices for fitting intensity in single-look images [1,5]. Additionally, the gamma, inverse gamma, G A 0 , and G I 0 distributions are well-known options for multi-look images [1]. However, to add flexibility and improve the goodness-of-fit for different settings of SAR image data, some flexible alternatives of probability distributions have been proposed in the literature (see, for instance, [6,7,8,9,10,11]), and are shown to be a practice of great relevance in the area.
In this sense, the goals of this paper are twofold. First, we introduce a four-parameter distribution as a SAR image descriptor. With the name of exponentiated transmuted inverted beta (ET-IB) distribution, the new model is obtained by extending the inverted beta (IB) distribution [12]. Known as beta prime, or beta distribution of the second kind, the IB distribution has been considered as a texture model for SAR image applications [13,14]. Our proposal generalizes the IB distribution from the exponentiated transmuted-G (ET-G) class [15]. The ET-G framework introduces two shape parameters in an existing distribution (baseline) to make it more flexible, especially for fitting asymmetric and heavy-tailed data. To the best of our knowledge, only a few studies generalize specific baselines on the ET-G family. For example, we can refer to Okereke [16] for the exponentiated transmuted Lindley distribution and Abbas et al. [17], who introduced the exponentiated transmuted length-biased exponential distribution. However, neither of them explored possible applications in SAR image modeling. Second, we show the suitability of the ET-IB distribution as a SAR descriptor by using simulated and measured amplitude images. The analysis focus on images related to forest, ocean, and urban regions. Moreover, the new model could be used for many applications, such as deforestation monitoring, crop growth, biomass quantification, military activity surveillance, maritime surveillance, oil slick detection, ship detection, search and rescue, and illegal activities monitoring [18,19,20,21]. In fact, the proposed ET-IB model can replace the IB distribution in any algorithm where it is appropriate. It is possible to improve the overall performance of the algorithm once the process of generalizing distributions tends to enhance the flexibility and goodness-of-fit of the baseline distribution. Using real SAR data, we compare the goodness-of-fit of the ET-IB distribution with its baseline and several classical statistical models for amplitude in SAR image interpretation. The results show that the proposed ET-IB distribution outperforms the competitor models.
Considering the above discussion, we summarize the contributions of the paper as follows:
  • A new probability model is proposed, which is an extension of an important texture model of SAR imagery;
  • The maximum likelihood theory is developed for parameter estimation;
  • Numerical experiments with synthetic signals are performed to validate the proposed model and inference theory;
  • Based on three measured SAR images, we show that the proposed model outperforms several well-known SAR image descriptors;
  • A collection of computational codes are available to guarantee reproducibility of the results and future applications of the proposal.
The rest of this paper is organized as follows. In Section 2, we present statistical preliminaries on the ET-G family and IB distribution, derive the proposed ET-IB distribution as a novel statistical tool for SAR image modeling, and discuss parameter estimation. Section 3 presents some possible applications for the ET-IB distribution. Finally, Section 4 provides conclusions and final remarks.

2. The Exponentiated Transmuted Inverted Beta Distribution

This section provides the necessary statistical background for understanding the derivation of the proposed ET-IB distribution.

2.1. Statistical Preliminaries

The random variable X with IB distribution has a probability density function (pdf) and a cumulative distribution function (cdf) that are given by [12]
g X ( x ; α , β ) = x α 1 ( 1 + x ) α β B ( α , β ) , x > 0 ,
and
G X ( x ; α , β ) = I x / ( 1 + x ) ( α , β ) = B ( x / ( 1 + x ) , α , β ) B ( α , β ) ,
respectively, where α , β > 0 ,   B ( a , b ) = Γ ( a ) Γ ( b ) / Γ ( a + b ) is the beta function, and Γ ( · ) is the gamma function. The beta and gamma functions are both efficiently implemented in several programming languages. I z ( a , b ) is the regularized incomplete beta function, and B ( z , a , b ) = 0 z t a 1 ( 1 t ) b 1 d t is the incomplete beta function. The parameters α and β control the shape and skewness of the IB distribution [22].
The ET-G family of continuous distributions was proposed to increase the flexibility of a baseline distribution [15]. The cdf and pdf for continuous ET-G distributions are given by
F X ( x ; ϕ , λ , ζ ) = G X ( x ; ζ ) ϕ 1 + λ λ G X ( x ; ζ ) ϕ ,
and
f X ( x ; ϕ , λ , ζ ) = ϕ g X ( x ; ζ ) [ 1 + λ 2 λ G X ( x ; ζ ) ] G X ( x ; ζ ) ϕ 1 1 + λ λ G X ( x ; ζ ) ϕ 1 ,
respectively, where ϕ > 0 and | λ | < 1 are the additional parameters of the ET-G family and ζ is the parameter vector of the baseline distribution with cdf G X ( x ; ζ ) .

2.2. The Model Description

The cdf of the ET-IB is defined by inserting (2) in (3), and is given by
F X ( x ; θ ) = I x / ( 1 + x ) ( α , β ) ϕ 1 + λ λ I x / ( 1 + x ) ( α , β ) ϕ ,
where x , α , β , ϕ > 0 , | λ | < 1 , and θ = ( α , β , ϕ , λ ) is the parameter vector. The corresponding pdf is
f X ( x ; θ ) = ϕ x α 1 I x / ( 1 + x ) ( α , β ) ϕ 1 ( 1 + x ) α + β B ( α , β ) 1 + λ 2 λ I x / ( 1 + x ) ( α , β ) 1 + λ λ I x / ( 1 + x ) ( α , β ) ϕ 1 .
Hereafter, a random variable with density (5) is denoted by X ET-IB ( α , β , ϕ , λ ) .
Some pdf plots are presented in Figure 1 to illustrate the effect of different parameter combinations in the new probability density function (5). The proposed pdf is suitable for modeling SAR images with asymmetry, positive skewness, heavy tail, and different degrees of variability, giving support to many SAR applications (see [2,4,9]). A shiny application that allows the reader to access dynamical plots with other parameter combinations and density shapes is available in [23].
Finally, by inverting (4), we obtain the quantile function of X, which is given by
Q ( u ; θ ) = 1 T λ ( λ + 1 ) 2 4 λ u 1 / ϕ + 1 2 λ , α , β 1 1 , for λ 0 , 1 T u 1 / ϕ , α , β 1 1 , for λ = 0 ,
where T ( u , α , β ) is the quantile function of the beta distribution with parameters α > 0 and β > 0 .
Considering the inversion method, if u is an observation of a uniform random variable on the unit interval, we can replace u in (6) to generate random numbers from the ET-IB distribution. Additionally, using (6), we can calculate the Bowley’s skewness ( S B ) [24] based on quartiles and the Moor’s kurtosis ( K M ) [25] based on octiles, given by
S B = Q ( 3 / 4 ; θ ) 2 Q ( 1 / 2 ; θ ) + Q ( 1 / 4 ; θ ) Q ( 3 / 4 ; θ ) Q ( 1 / 4 ; θ )
and
K M = Q ( 7 / 8 ; θ ) Q ( 5 / 8 ; θ ) Q ( 3 / 8 ; θ ) + Q ( 1 / 8 ; θ ) Q ( 6 / 8 ; θ ) Q ( 2 / 8 ; θ ) .

2.3. Likelihood Inference

In practice, the parameters of the ET-IB distribution are usually unknown and need to be estimated. In this study, we consider the maximum likelihood theory for this purpose due to the easy obtainment and good properties, such as consistency and asymptotic efficiency of the maximum likelihood estimator (MLE) (see [26], for more information).
Let x 1 , , x n be a signal of length n from X ET-IB ( α , β , ϕ , λ ) . The MLE of θ is given by
θ ^ = arg max θ Θ ( θ ) ,
where θ ^ = ( α ^ , β ^ , ϕ ^ , λ ^ ) , Θ is the parametric space of θ , and
( θ ) = i = 1 n log ( f X ( θ | x i ) ) = n log ( ϕ ) + ( α 1 ) i = 1 n log ( x i ) ( α + β ) i = 1 n log ( 1 + x i ) + ( ϕ 1 ) i = 1 n log I x i / ( 1 + x i ) ( α , β ) + i = 1 n log 1 + λ 2 λ I x i / ( 1 + x i ) ( α , β ) + ( ϕ 1 ) i = 1 n log 1 + λ λ I x i / ( 1 + x i ) ( α , β )
is the log-likelihood function of θ for the observed signal.
Differentiating (7) with respect to each unknown parameter, we obtain the score vector
U ( θ ) = ( θ ) α , ( θ ) β , ( θ ) ϕ , ( θ ) λ .
These components are given by
( θ ) α = i = 1 n log x i i = 1 n log x i + 1 i = 1 n 2 λ K ( x i , α , β ) 1 + λ 2 λ I x i / ( 1 + x i ) ( α , β ) + ( ϕ 1 ) i = 1 n K ( x i , α , β ) I x i / ( 1 + x i ) ( α , β ) ( ϕ 1 ) i = 1 n λ K ( x i , α , β ) 1 + λ λ I x i / ( 1 + x i ) ( α , β ) ,
( θ ) β = ( ϕ 1 ) i = 1 n V x i , α , β I x i / ( 1 + x i ) ( α , β ) i = 1 n log x i + 1 λ ( ϕ 1 ) i = 1 n V x i , α , β 1 + λ λ I x i / ( 1 + x i ) ( α , β ) 2 λ i = 1 n V x i , α , β 1 + λ 2 λ I x i / ( 1 + x i ) ( α , β ) ,
( θ ) ϕ = n ϕ + i = 1 n log I x i / ( 1 + x i ) ( α , β ) + i = 1 n log 1 + λ λ I x i / ( 1 + x i ) ( α , β ) ,
( θ ) λ = i = 1 n λ + 1 1 2 I x i / ( 1 + x i ) ( α , β ) 1 + ( ϕ 1 ) i = 1 n λ + 1 1 I x i / ( 1 + x i ) ( α , β ) 1 ,
where
K ( x i , α , β ) = I x i / ( 1 + x i ) ( α , β ) log x i / ( 1 + x i ) + ψ ( α + β ) ψ ( α ) Γ ( α ) 2 x i / ( 1 + x i ) α Γ ( α + 1 ) 2 B ( α , β ) × 3 F 2 α , α , 1 β ; α + 1 , α + 1 ; x i / ( 1 + x i ) ,
V ( x i , α , β ) = I 1 / ( 1 + x i ) ( β , α ) ψ ( β ) ψ ( α + β ) log 1 / ( 1 + x i ) + 1 / ( 1 + x i ) β β 2 B ( α , β ) × 3 F 2 1 α , β , β ; β + 1 , β + 1 ; 1 / ( 1 + x i ) ,
ψ ( z ) = Γ ( z ) / Γ ( z ) is the digamma function, Γ ( z ) is the gamma function, and p F q ( a ; b ; z ) is the generalized hypergeometric function.
The MLEs of θ are obtained by taking U ( θ ) = 0 , where 0 is a null vector of dimension four. The solution cannot be expressed in closed form. However, we can obtain θ ^ using a Broyden–Fletcher–Goldfarb–Shanno (BFGS) optimization algorithm implemented in the R programming language [27].

3. Numerical Results

In this section, synthetic and measured SAR amplitude images corresponding to forest, ocean, and urban regions are modeled by the proposed distribution. Usually, these types of regions are modeled as clutters in target detection and classification problems, which are considered relevant research topics in statistical SAR image processing [28]. All the implementations and numerical experiments are made in R language. The R codes with a function to fit the ET-IB model are available in [29]. In addition, we also provide the pdf, cdf, quantile function, and a function for generating pseudo-random numbers of the ET-IB distribution.

3.1. Analysis with Simulated Data

Monte Carlo simulations are performed to assess the MLE performance for finite signal lengths. We consider the following metrics: mean estimates, bias, standard deviation (SD), and total relative bias (TRB), defined as the sum of the absolute measures of the relative biases. The parameters used for the simulations were defined from the fit of ET-IB distribution in the measured SAR images presented in Section 3.2. Considering three different scenarios with θ = (6.3, 36.2, 0.4, −0.9 ) , θ = (3.0, 37.5, 3.7, 0.8 ) , and θ = (0.4, 5.3, 66.9, 0.9 ) , we simulate single-look and multi-look SAR amplitude images, related to forest, ocean, and urban regions, respectively. In all scenarios, we simulate 10,000 patches with dimensions 60 × 60, 90 × 90, and 120 × 120 pixels.
The simulation results are summarized in Table 1. As expected, the MLEs converge to the true values of θ , and the bias, the SD, and TRB gradually converge to zero as the image dimensions increase. Notice that the speed of convergence differs among the scenarios. The TRB decays faster in the forest region, which is also the scenario with more accurate estimates (lower relative biases). Meanwhile, the urban region is the one with the slowest convergence. In general, we can see a good performance of the estimators even in moderate signal lengths, validating the developed estimation theory. It reveals that the ET-IB distribution performs well also for small SAR image patches.

3.2. Analysis with SAR Amplitude Data

We used three datasets to assess the performance of the proposed ET-IB distribution in SAR image modeling.
Figure 2a is a single-look amplitude SAR image, with HH polarization, with dimensions of 90 × 90 pixels, representing a forest region in northern Sweden. This image belongs to a dataset acquired with the CARABAS-II system. The CARABAS-II system is a Swedish ultrawideband (UWB) very-high frequency (VHF) SAR system (for more information, see [30]). Figure 2b,c are four-look SAR images referring to the ocean and urban regions of San Francisco, California, respectively. Figure 2b,c have dimensions of 75 × 50 pixels and 30 × 150 pixels. Those images were acquired with the Airborne Synthetic Aperture Radar (AIRSAR) sensor in L-band (see [31] for more information).
Table 2 presents descriptive measures of the considered datasets, such as mean, median, maximum (max.), minimum (min.), coefficients of variation (CV), skewness (CS), and kurtosis (CK). The lower mean and median values in the ocean region may indicate a lower backscatter in the same area. They also present a lower CV. This may be because four looks in the image generation attenuate the noise. The increase in the number of looks tends to mitigate the variability [32]. Furthermore, the high variability of the dataset in the urban region is probably due to the presence of different elements in the scene, such as streets and houses. Finally, the high values of CS and CK of the three datasets are common features in SAR images, since they usually present long and fat tails [33].
For each dataset, we fit the ET-IB distribution and the following competitor models: the IB, Rayleigh, Weibull, log-normal, Rician, K, and G A 0 distributions. To evaluate and compare the adjustments, we present the number of parameter (NP) and computed the following goodness-of-fit (GoF) statistics: the Akaike Information Criterion (AIC) [34], corrected statistic of Cramér–von Mises (W*), and the Kolmogorov–Smirnov (K-S) test. They are calculated using the goodness.fit function from the AdequacyModel package [35] in the R statistical computing environment. The distribution with the smallest GoF measures is the one that best fits the dataset. We also presented the p-value of the K-S test, where the null hypothesis is that the sample is drawn from the reference distribution.
Table 3 presents the GoF measures for all fitted models for all types of regions. These measures evidence the superiority of the ET-IB over the classical SAR amplitude image distributions. According to all GoF measures, the best fit is provided by the ET-IB distribution for all three regions. Among the usual distributions, the G A 0 stood out as the only one besides the ET-IB which did not reject the null hypothesis in the K-S test at 5 % of significance level (p-value greater than 0.05). The results highlight the importance of the two additional parameters of the ET-G family for obtaining a distribution with consistently better performance than its baseline in SAR applications.
Graphical representations of the estimated log-densities of each considered distribution and the log-frequency for each dataset are presented in Figure 3. As expected, the new distribution properly fits the long and fat tails of the three considered datasets. Therefore, the practical importance of the ET-IB distribution as a SAR image descriptor is observed in the current applications. It turned out to be a reliable alternative for modeling pixel amplitude values of single-look and multi-look images characterized as forest, ocean, and urban regions, respectively. In this way, it reveals the potential to compete with the usual distributions to describe these and other types of SAR images, aiming to detect target- and ground-type changes, land classification, etc.

4. Conclusions

This paper introduced a new probability density function as a SAR image descriptor named exponentiated transmuted-inverted beta (ET-IB) distribution. We presented important statistical properties of the ET-IB distribution and discussed parameter estimation. The proposed distribution was validated with numerical experiments based on simulated and measured data for modeling forest, ocean, and urban regions in SAR amplitude images. The ET-IB overcomes the baseline distribution in terms of fit performance limitations. Moreover, the proposed ET-IB distribution is adequate for modeling amplitude, single-look, and multi-look data due to the flexibility provided by the additional ET-G family shape parameters. The proposed distribution also works well for the intensity format. Pilot simulations showed that the proposed model outperforms some usual distributions for SAR intensity images according to the GoF measures and log-frequency plot. However, due to simplicity and results similarities, we did not include the results from intensity images in this paper. In summary, the proposed ET-IB distribution showed to be a versatile statistical model for SAR image description. In future works, the ET-IB distribution can serve as an input for several algorithms applicable to SAR image processing, such as regression models, time-series models, and control charts, which useful in several SAR problems such as edge detection, data exploitation, ship detection, segmentation, restoration, pattern recognition, classification, target recognition, change detection, and anomaly detection, as similarly discussed in [2,4,21,30,31,36,37,38,39,40,41,42].

Author Contributions

Conceptualization, M.S., R.R.G. and F.M.B.; methodology, M.S., R.R.G., F.M.B. and R.M.; software, M.S., R.R.G., F.M.B. and R.M.; validation, M.S., R.R.G., F.M.B. and R.M.; formal analysis, M.S.; investigation, M.S., R.R.G., F.M.B. and R.M.; resources, M.S., R.R.G., F.M.B. and R.M.; data curation, M.S.; writing—original draft preparation, M.S., R.R.G., F.M.B. and R.M.; writing—review and editing, M.S., R.R.G., F.M.B. and R.M.; visualization, M.S., R.R.G., F.M.B. and R.M.; supervision, R.R.G., F.M.B. and R.M.; project administration, R.R.G., F.M.B. and R.M.; funding acquisition, M.S., R.R.G., F.M.B. and R.M. All authors have read and agreed to the published version of the manuscript.

Funding

This research was partially supported by the Brazilian agencies Coordination for the Improvement of Higher Education Personnel (CAPES), National Council for Scientific and Technological Development (CNPq), and São Paulo Research Foundation (FAPESP) under grant #2020/09838-0 (BI0S—Brazilian Institute of Data Science).

Data Availability Statement

The data are available at https://www.sdms.afrl.af.mil/index.php, accessed on 5 May 2022 and https://ietr-lab.univ-rennes1.fr/polsarpro-bio/san-francisco/, accessed on 5 May 2022.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. Examples of density formats of the ET-IB distribution for α = 0.8 .
Figure 1. Examples of density formats of the ET-IB distribution for α = 0.8 .
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Figure 2. Images used in measured SAR data applications: (a) single-look VHF UWB SAR image referring to a forest region in northern Sweden, (b,c) four-look L-band SAR images referring to the ocean and urban areas, respectively, from San Francisco, California.
Figure 2. Images used in measured SAR data applications: (a) single-look VHF UWB SAR image referring to a forest region in northern Sweden, (b,c) four-look L-band SAR images referring to the ocean and urban areas, respectively, from San Francisco, California.
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Figure 3. Log-frequency and estimated log-density of the ET-IB and competitor distributions for (a) forest region, (b) ocean region, and (c) urban region.
Figure 3. Log-frequency and estimated log-density of the ET-IB and competitor distributions for (a) forest region, (b) ocean region, and (c) urban region.
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Table 1. Monte Carlo results: mean of maximum likelihood estimates, bias, sd, and TRB.
Table 1. Monte Carlo results: mean of maximum likelihood estimates, bias, sd, and TRB.
Scenario
Forest ( α , β , ϕ , λ ) (6.3, 36.2, 0.4, −0.9)
n × n 60 × 6090 × 90120 × 120
mean(6.46, 36.76, 0.40, −0.89) (6.36, 36.40, 0.40, −0.90) (6.33, 36.29, 0.40, −0.90)
Bias(0.16, 0.53, 0.00, 0.00) (0.06, 0.20, 0.00, 0.00) (0.03, 0.09, 0.00, 0.00)
SD(0.68, 2.42, 0.06, 0.05) (0.43, 1.56, 0.04, 0.03) (0.35, 1.19, 0.03, 0.05)
TRB0.060.020.01
Ocean ( α , β , ϕ , λ ) (3.0, 37.5, 3.7, 0.8)
n × n 60 × 6090 × 90120 × 120
mean(2.89, 37.28, 4.26, 0.78) (2.94, 37.23, 3.95, 0.79) (2.98, 37.47, 3.81, 0.80)
Bias(−0.11, −0.22, 0.56, −0.02) (−0.06, −0.27, 0.25, 0.00) (−0.02, −0.03, 0.11, 0.00)
SD(0.56, 5.66, 1.54, 0.11) (0.39, 4.15, 0.87, 0.07) (0.31, 3.27, 0.59, 0.05)
TRB0.220.100.04
Urban ( α , β , ϕ , λ ) (0.4, 5.3, 66.9, 0.9)
n × n 60 × 6090 × 90120 × 120
mean(0.46, 5.28, 54.04, 0.89) (0.44, 5.29, 59.60, 0.90) (0.43, 5.31, 60.96, 0.90)
Bias(0.06, −0.02, −12.86, −0.01) (0.04, 0.00, −7.30, 0.00) (0.03, 0.01, −5.94, 0.00)
SD(0.09, 0.43, 17.31, 0.03) (0.07, 0.29, 17.63, 0.02) (0.06, 0.21, 17.33, 0.02)
TRB0.360.210.18
Table 2. Summary statistics of datasets.
Table 2. Summary statistics of datasets.
DatasetMin.Max.MeanMedianCV(%)CSCK
Forest region7.72 × 10 4 0.620.150.1454.450.924.32
Ocean region0.020.320.100.0941.191.476.25
Urban region0.093.750.450.3768.863.2121.22
Table 3. GoF measures for different probability distributions considering the forest, ocean, and urban region datasets. The best results are presented in bold font.
Table 3. GoF measures for different probability distributions considering the forest, ocean, and urban region datasets. The best results are presented in bold font.
ScenarioModelNPAICW*KS (p-Value)
ForestET-IB4−18,752.340.0280.005 (0.973)
IB2−18,468.013.9230.040 (<0.001)
Rayleigh1−18,658.600.7320.021 (<0.001)
Weibull2−18,680.150.6020.017 (0.014)
Log-normal2−17,521.4015.1390.108 (<0.001)
Rician2−18,656.600.7320.021 (<0.001)
K2−18,722.740.2990.017 (0.022)
G A 0 3−18,735.880.2480.012 (0.180)
OceanET-IB4−14,354.080.1100.013 (0.456)
IB2−14,215.732.0230.047 (<0.001)
Rayleigh1−13,194.106.8110.115 (<0.001)
Weibull2−13,536.559.6900.083 (<0.001)
Log-normal2−14,329.520.5010.843 (<0.001)
Rician2−13,432.6811.5440.090 (<0.001)
K2−13,158.915.7200.157 (<0.001)
G A 0 3−14,350.440.1170.015 (0.348)
UrbanET-IB4−1418.990.0300.008 (0.927)
IB2−1072.494.3010.054 (<0.001)
Rayleigh1633.1122.5170.161 (<0.001)
Weibull2181.2117.0770.105 (<0.001)
Log-normal2312.870.3810.484 (<0.001)
Rician2635.1122.5170.161 (<0.001)
K2−321.2211.4060.091 (<0.001)
G A 0 3−1406.310.0920.012 (0.543)
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Sagrillo, M.; Guerra, R.R.; Bayer, F.M.; Machado, R. A New Probability Distribution for SAR Image Modeling. Remote Sens. 2022, 14, 2853. https://doi.org/10.3390/rs14122853

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Sagrillo M, Guerra RR, Bayer FM, Machado R. A New Probability Distribution for SAR Image Modeling. Remote Sensing. 2022; 14(12):2853. https://doi.org/10.3390/rs14122853

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Sagrillo, Murilo, Renata R. Guerra, Fábio M. Bayer, and Renato Machado. 2022. "A New Probability Distribution for SAR Image Modeling" Remote Sensing 14, no. 12: 2853. https://doi.org/10.3390/rs14122853

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Sagrillo, M., Guerra, R. R., Bayer, F. M., & Machado, R. (2022). A New Probability Distribution for SAR Image Modeling. Remote Sensing, 14(12), 2853. https://doi.org/10.3390/rs14122853

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