1. Introduction
Marine radar plays a crucial role in target detection, rainfall detection, wind field inversion, and wave inversion, due to its advantages of being unaffected by weather, environment, and space range [
1,
2,
3,
4,
5,
6]. Since the presence of both target and sea clutter signals in the backscattered radar signal, effectively detecting the target with marine radar in complicated sea clutter conditions is faced with significant challenges. At present, the X-band marine radar target detection methods can be divided into two categories: constant false alarm rate (CFAR) of target detection and tracking before detection (TBD) of target tracking [
7].
Among these, CFAR detection stands out as the most widely employed radar target detection method. It involves initial statistical analysis and the modeling of sea clutter amplitude, followed by the finding of an optimal or sub-optimal detector to achieve the final detection. According to different detection processes, CFAR can be divided into four categories: the first category is direct CFAR detection, the second category is non-adaptive filtering-then-CFAR detection, the third category is adaptive filtering-then-CFAR detection, and the fourth category is adaptive CFAR detection [
8]. Only the CFAR detector for point-by-point detection without a filtering process is utilized in the first kind of method, and the detection performance is inadequate. Moving target indication (MTI) [
9] and moving target detection (MTD) [
10] both belong to the second kind of CFAR. The detection scheme is typically less intricate than the third kind of CFAR, whereas the limited filtering performance results in a certain degradation in detection efficiency. By combining sea clutter suppression methods such as space-time domain sea clutter suppression (STCS) [
11], eigenvalue decomposition (EVD) [
12], and empirical mode decomposition (EMD) with CFAR detection, the third category CFAR has numerous advantages. In this method, the signal-to-clutter ratio (SCR) of the output filtered data are adaptively maximized, and a CFAR detector for the filtered data are designed to complete target detection. The fourth category CFAR obviates the need for independent filtering processes, integrating the filtering process within the CFAR detection process, thereby being embedded in the adaptive detection statistical analysis [
13]. Such methods mainly include KGLRT [
14] and AMF [
15]. Although the four categories CFAR detection methodologies differ from one another, the key to achieve efficient detection of sea surface targets lies in the application of a highly matching degree sea clutter statistical model and a superior performance detector.
Consequently, the mastery of the optimal sea clutter statistical distribution is considerable for constructing appropriate target detection schemes. The sea clutter generation involves a complex physical mechanism that is influenced by various factors, including the sea state and marine meteorology [
16]. As a consequence, sea clutter exhibits intricate characteristics such as being non-uniform, non-Gaussian, and non-stationary, along with exceedingly complex space-time variability [
17]. In numerous prior studies, various distributions have been proposed to model the statistical characteristics of data acquired from diverse environments, including the Weibull distribution, Log-normal distribution, K distribution, Generalized Pareto (GP) distribution, mixed distribution of K and K (KK), and mixed distribution of Weibull and Weibull (WW) [
18,
19,
20,
21,
22,
23]. Due to, but not limited to, significant variations in the sea spike amplitude distributions across different sea states, the aforementioned distribution can not accurately adapt the real sea clutter amplitude distribution under all conditions. If the sea clutter model is inaccurate, the performance of the detector designed based on the hypothetical statistical model will be observably diminished. In order to address the issue of unstable matching between the distribution model and the real background clutter distribution caused by the space-time changes in sea clutter, the space-time adaptive filter suppression method (STAF) [
24] was introduced into the statistical analysis of sea clutter distribution. Through utilizing the sea clutter dispersion characteristics in the three-dimensional frequency wave-number domain, as well as the wave velocity feature of moving targets in the same domain, STAF adaptively suppresses sea clutter and extracts targets. The introduction of STAF into sea clutter distribution statistics is driven by its ability to leverage filtered background clutter in modeling the required clutter distribution for subsequent CFAR process. Simultaneously, STAF can serve as an adaptive filtering component in the filtering-then-CFAR detection scheme. The approach not only maximizes the output SCR, but also mitigates the impact of fluctuating distribution models caused by space-time sea clutter variations, thereby obtaining the data with high SCR and a uniformly stable background amplitude distribution.
The generalized extreme value (GEV) distribution is utilized to model the probability of extreme event occurrences. For this reason, GEV is employed for fitting SAR radar images in both uniform and non-uniform environments, as well as for implementing global CFAR detection in [
25,
26,
27]. Furthermore, GEV is utilized to model the sea spike component in low grazing angle marine radar and to construct a comprehensive background distribution weighted with the non sea spike component modeled by other distribution models [
28]. The background clutter in the filtered image is no longer influenced by a large number of sea spikes and near-far effects, retaining only a small portion sea peaks. This deviates somewhat from traditional distributions, but exhibits certain similarity with SAR radar images in a uniform environment. Accordingly, the GEV distribution is introduced to statistically model the entire space-time filtering background clutter distribution of marine radar maps.
The selection of an excellent detector is a crucial aspect of the CFAR detection. The CFAR detector can dynamically determine the threshold based on the known background clutter distribution and the preset false alarm rate, which is a function of the selected background clutter statistical distribution [
29]. Over the years, multitudinous sliding window CFAR detectors have been proposed for incoherent scanning radar. Ranging from the earliest cell mean (CA) to ordered statistics (OS), it has been demonstrated to exhibit better detection performance in uniform and non-uniform environments, respectively [
30,
31]. The Log-t detector has been validated to maintain CFAR properties in Log-normal and Weibull distributions [
32]. The later proposed Inclusion/Exclusion (IE) method establishes decision rules by excluding a portion reference unit and selecting another portion for participation in clutter level estimation [
33]. The decision rule in Weber–Haykin (WH) is determined by selecting two units from reference units to participate in clutter level estimation [
34]. A first-order statistic is added in Weber–Haykin-ordered statistics (WHOS) based on WH to implement the decision rule, and three units are selected for participation in clutter level estimation [
35]. By selecting a portion of the reference unit and the kth order statistic of reference units to participate in clutter level estimation, the decision rule is established in trim average ordered statistics (TMOS) [
36]. Geometric average ordered statistics (GMOS) establishes decision rules by combining all reference units with the kth order statistic within reference units [
37]. The CFAR properties of these detectors have been demonstrated under Weibull distribution, mixed Weibull distribution, and Pareto Type I distribution [
38,
39,
40].
Due to the fact that the detection link in the proposed STAF-RCBD-CFAR is not a CFAR detector under clutter modeling, but a global threshold CFAR detector, its detection performance for low SCR target edge points is not satisfactory. In order to address this issue, this paper first improves the original two-stage detection STAF-RCBD-CFAR method by designing a CFAR detector under clutter backgrounds based on filtered imagery. The design process encompasses two key components: the first component involves conducting a statistical analysis of the clutter background subsequent to STAF filtering, while the second component pertains to selecting the optimal detector tailored to the distribution of the clutter background post-STAF filtering. The statistical analysis of radar clutter backgrounds under varying conditions, utilizing known distributions, has been one of the research topics continuously pursued in recent decades. This article presented a statistical analysis of background clutter filtered by STAF, employing Log-normal, Weibull, K, Generalized Pareto, KK, WW distributions, and GEV distributions. Due to the absence of sea clutter, the conventional sea clutter model proves to be inapplicable. The introduced GEV distribution demonstrates superior fit due to its characteristic of containing a small amount of extreme clutter in a large number of uniform clutters. Although GEV has previously been utilized in SAR radar’s sea clutter distribution fitting, it is important to note that the imaging mechanisms between SAR and maritime radars are fundamentally different. Meanwhile, the existing literature predominantly employs GEV theory for fitting sea clutter peaks or distributions under specific conditions (such as non-uniform or uniform multi-target scenarios), rather than focusing on global clutter distribution fitting that effectively filters out sea clutter. Regarding the research on the second aspect, evaluating the detection performance of known detectors under different distributions remains a key research topic. To date, there has been no investigation into the detection performance of these CRP-CFAR methods under the GEV distribution. This paper employed multiple background clutter datasets characterized by the GEV distribution to evaluate and analyze the performance of various detectors, ultimately identifying the optimal detector within the STAF-GEV distribution model. The innovative contributions of this paper can be summarized as follows.
1. This article presented, for the first time, a statistical analysis of background clutter filtered by STAF, employing Log-normal, Weibull, K, Generalized Pareto, KK, WW distributions, and GEV distributions. In the process of statistical analysis and modeling, it has been demonstrated from multiple aspects, such as the global fitting effect and local tailing fitting effect of CDF and PDF, that GEV is the best model.
2. In selecting the most optimal detector, the performance of each detector was rigorously evaluated using detection curves, establishing that IE-CFAR exhibits effectiveness and superior performance under this framework.
3. For the first time, the adaptive filtering in the frequency-wavenumber domain (or time-space domain) is combined with CFAR detection under background clutter. This approach effectively resolves the issue of inadequate detection of low SCR target edge points that arises from employing global CFAR detection within the STAF-RCBD-CFAR method. Additionally, it mitigates performance degradation caused by complex and variable sea clutter during CFAR detection. In comparison to the STAF-RCBD-CFAR method, the proposed STAF-GEV-IE-CFAR method demonstrates superior detection performance.
The remainder of this article is structured as follows:
Section 2 provides a brief overview of the original data utilized in the experiment, details on the filtering process, and filtered data. Furthermore, the filtered data distribution modeling is discussed. In
Section 3, six types of incoherent CRP-CFAR detectors are comprehensively presented. In
Section 4, the detection performance of proposed algorithm is evaluated by using real data.
Section 5 discusses the proposed method, and
Section 6 summarizes the content of the article.
2. Background Clutter Distribution Modeling
In this section, real marine radar data under varying sea states, times and regions are selected to obtain clutter background distribution modelings. Subsequently, the three-dimensional (3D) frequency wave-number domain adaptive filtering method is briefly outlined, followed by an analysis of the filtered clutter background distribution modeling results. Finally, a unified generalized extreme value distribution model is established to characterize the filtered data under various conditions, and the effectiveness of the model is validated.
2.1. Original Marine Radar Data
The experimental data were obtained from the marine datasets in the East China Sea, and the datasets were collected by X-band ship-based radar in October 2017. The radar pertains to the mono pulse scanning marine radar, which has a height of 25 m, a grazing angle of 0.22 degrees, and a rotation time of around 2.3 s. A single radar map consists of 2048 lines, with each line containing 600 range bins and covering a radial distance of 4.5 km. The wave height of the selected datasets (the average height of the one-third of highest waves) range from 1.5 m to 3.5 m. The square region incised in the PPI map is transformed from polar coordinates to Cartesian coordinates by employing the nearest neighbor interpolation method. The pixels of the interpolation map are 848 × 848.
The interpolated original maps of three distinct wave heights are depicted in
Figure 1. The whole map contains data collected along lines perpendicular and parallel to the wave direction. The upwave data exhibited more pronounced spike characteristics, which differed significantly from the crosswave data. Secondly, the electromagnetic wave transmitted by the radar antenna will experience attenuation when propagating in the air, resulting in near and far effects which, in turn, leads to cause variations in sea clutter distribution within the same map. Accordingly, the original map data were divided into different regions and the sea clutter distributions were calculated. The area where both the central saturation zone and radar blind area have been removed in the whole region. Subsequently, the whole area was categorized into the near region and far region based on radial distance.
Figure 2a,b display the statistical sea clutter probability density function (PDF) and cumulative distribution function (CDF) for the whole region, near region, and far region in three data. With the increase in wave height, the sea clutter PDF shifts toward higher gray values as a whole. Furthermore, the proportion of high gray values increases, leading to a slower rate at which the CDF of sea clutter reaches 1 and a larger trailing effect. The sea clutter in the near region possesses a higher overall gray value, with larger trailing in both the PDF and CDF. Conversely, the sea clutter in the far region displays a weaker overall gray value, with smaller trailing in the PDF and CDF. Furthermore, sea clutter PDF and CDF exhibit significant differences in both near and far regions, as well as across the whole region. Hence, it is essential to process the raw data in order to achieve a consistent and homogeneous background clutter distribution.
2.2. Space-Time Adaptation Filtering
The original data are processed by STAF [
24]. First, the raw image sequence
is transformed to a 3D frequency wave-number spectrum
by 3D fast Fourier transform (FFT). The discrete form of this spectrum is expressed as follows:
where
and
are the spatial scales of the image sequence, and
T denotes the temporal scale.
and
denote the wave-number components of the spectrum,
is the temporal frequency, and
is the 3D frequency wave-number image spectrum. The resolutions of the wave-number components and frequency are
,
, and
.
The upper and lower boundaries of the filter are established based on the dispersion relationship under the dominant wavelength of sea clutter.
where
and
refer to the upper and lower boundaries of frequency band of the filter, respectively.
where
represents the sea clutter suppression image spectrum.
Subsequently, two wave-number planes in
E are chosen for Hough detection, and two sets of Hough parameters are employed to establish the background clutter filter model as follows:
where
and
represent all line slopes and intercepts separately detected by the Hough transform.
n represents the index of a wave-number spectrum in the frequency wave-number domain,
a and
b represent the sequence numbers of the two selected images, and
is the width expansion coefficient. In this study,
is set to 20.
3D-IFFT is applied to
, and the processed image sequence is obtained.
As depicted in
Figure 3, the processed images validate the space-time filtering results. The marine radar image can be seen a significant reduction in sea peak and a consistent clutter background across all regions after clutter suppression, effectively mitigating the influence of near and far effects. The background clutters are composed of most of homogeneous clutter with a few intense clutter, demonstrating uniformity and consistency.
The statistical clutter PDF and CDF for the three datasets are depicted in
Figure 4, with each dataset further divided into three kinds to illustrate the situation in different regions. The gray value of the peaks in the PDF for far areas is approximately 190, while it reaches about 280 for near regions and around 200 for the whole area. The gray values range from 600 to 750 when the CDF reaches 1 in these three regions. The overall shape and tail of the clutter distribution remains consistent across various wave heights, and the difference in distinct regions is effectively diminished.
2.3. Filtered Background Clutter Distribution Modeling
The GEV distribution, derived from the limit theorem in extreme value theory, is employed to characterize the probability of extreme events and is frequently utilized for modeling extreme phenomena. In the preceding section, it was determined that the filtered background clutter distribution conforms to a uniform clutter with tiny extreme clutter, thereby a theoretical foundation is established for employing the GEV distribution in modeling.
Assuming that
is an independent and identically distributed random variable, and
denotes the maximum value among these variables, extreme value theory pertains to the distribution of
as
n approaches infinity. In accordance with the limit theorem, the distribution of the maximum
tends to converge towards a non-degenerate distribution function under appropriate linear transformations, specifically the generalized extreme value distribution. There exists a constant of normalization
and
[
41]:
where
is the CDF function of the GEV distribution. The GEV distribution comprises three subtypes of extreme value distributions: Gumbel extreme value distribution, Frechet extreme value distribution, and Weibull extreme value distribution. A standardized structure is described for the three distributions.
The position parameter is denoted by , the scale parameter is denoted by , and the shape parameter is denoted by . Moreover, . When , it corresponds to the extreme value distribution of type II Frechet, and exhibits heavy-tailed behavior. When , it corresponds to the type I Gumbel extreme value distribution, characterized by exponential tail decay. When , it corresponds to the Weibull extreme value distribution of type III and possesses a bounded upper tail. F represents the CDF of the GEV, while f denotes its PDF.
2.4. Distribution Model Analysis
The Rayleigh distribution is initially employed to fit the sea clutter background distribution in low resolution marine radars. With the enhancement of radar resolution and reduction in grazing angle, the sea clutter distribution no longer adheres to Rayleigh, but instead conforms to complex distributions such as compound Gaussian (CG) distribution. Log-normal, Weibull, K, GP, KK, and WW are proposed successively, and the conformity with the sea clutter distributions are demonstrated under diverse conditions. The Log-normal distribution and Weibull distribution can effectively modulate the distribution shape via their parameters, rendering them well-suited for diverse clutter models and demonstrating strong universal applicability. Nevertheless, the tail fitting capability for heavy-tailed clutter is unsatisfactory. The K distribution, arising from the convolution of Rayleigh and Gamma distributions, commendably characterizes clutter with spikes and heavy tails; however, the parameter estimation process is intricate. The GP distribution is appropriate for modeling the tail region of a distribution containing extreme values, whereas it cannot provide sufficient accuracy for modeling the data central part. The KK and WW distributions of dual population distributions gain the capability to effectively model complex structures by blending two identical distributions in proportion, but precise parameters are essential for ensuring consistency. To ensure precision, over 20 million data points in each datasets was employed for parameter estimation. In this paper, MLE is applied for parameter estimation of the Log-normal, Weibull, GP, and GEV distributions. Additionally, MoM is employed for parameter estimation of the K, KK, and WW distributions. Given that the probability of detection is influenced by the entire distribution region and the detection threshold is determined by the tail region, the overall goodness of fit (GoF) for the clutter PDF distribution and the local GoF for the tail region of the CDF distribution are assessed.
To determine the appropriate entirety distribution model, various overall GoF tests are employed, including the mean square error (MSE) test and Kolmogorov–Smirnov (KS) test. The error GoF is utilized for testing the local GoF in order to determine an appropriate local distribution model.
where
is the estimated value based on real data, and
is the value of the theoretical distribution.
where
is the estimated value based on real data, and
is the value of the theoretical distribution.
Figure 5 illustrates the fit results of each distribution to the three set processed data. As shown in
Figure 5a,c,e, the result is successively the GEV, WW, and Weibull distributions in descending order of GOF. The second echelon is the Log-normal distribution, and the third echelon is the K and KK distributions. And as expected, the GP distribution is the worst. A similar result is evident in
Figure 5b,d,f with regard to the CDF fit of the data.
Table 1 and
Table 2 present the evaluation values for each distribution regarding the fitting effect of PDF and CDF, respectively. The KS and MSE values of the GEV distribution are minimum during the fitting process, indicating the highest level of GOF, consistent with the findings from previous analysis. The KS and MSE values of WW and Weibull distributions demonstrate a marginal increase in comparison to the GEV, reflecting the universal applicability of Weibull distributions. The K and KK distributions exhibit large KS and MSE values, which can be attributed to the attenuation of the sea spike in the processed data. Owing to the inadequate suitability for whole distribution fitting, the GP distribution demonstrates the highest KS and MSE values, signifying the poorest fit.
In addition to focusing on the overall fit of each distribution, it is imperative to also evaluate the GoF in the local tail region. A comparison of the GoF in the local tail regions for each distribution is presented in
Figure 6 and
Table 3. The GEV distribution tail region is highly consistent with the data PDF and CDF tail region. In the selected range of
from 0.9 to 0.9999, only 0.9999 of the first group and 0.99 of the second group exhibit slightly lower values compared to other distributions, ranking second in terms of performance. For the tail region as a whole, the Weibull distribution shows slightly inferior performance to the GEV distribution and ranks second. The WW distribution ranks third due to its composition of two Weibull distributions. The remaining distributions display relatively large deviations in their tail regions. From the perspective of the scattering mechanism, the discrepancy can be understood. In composite Gaussian model, large-scale gravity waves and small-scale capillary waves as scattering events are considered, corresponding to texture and speckle components, respectively. Because of the elimination of most sea peaks and sea clutter during the filtering process, the current composite Gaussian model is unable to accurately signify the tail region. The experimental data demonstrate that the GEV distribution is suitable for modeling not only the local sea clutter peak distribution, but also the entire background clutter distribution. In
Section 4, further validation of the GEV as a background clutter distribution model filtered in the 3D frequency wave-number domain.
3. Incoherent Clutter Range Profile CFAR Detector
The CPR-CFAR detector is a spatial domain processor, and its principles are illustrated in
Figure 7. The decision rule assumes that
represents a set of independent identical distribution (iid) clutter statistics known as clutter range profile, where
denotes the cell under test (CUT). After excluding the guard units, CRP encompasses statistics
and
on both sides. The clutter gray value level are acquired through the utilization of two scale-invariant functions
and
to calculate these statistical parameters. Subsequently, a clutter gray value level measurement is obtained by applying the scale-invariant function
g [
42]. Ultimately, the constant normalized factor
is employed to generate an adaptive threshold, ensuring a consistent false alarm rate. By comparing the statistical parameters of the CUT with the final threshold
T, it can determine whether a target is detected in the CUT.
When the clutter model follows a scale and power invariant distribution, the adaptive detection threshold can be expressed in the following general form of the test [
33]:
When the gray value of detection unit exceeds the detection threshold, it is categorized as a target point and denoted as . Conversely, if the gray value falls below the detection threshold, it is classified as background clutter point and denoted as .
The CRP-CFAR detectors that conform to Formula (
15) include Logt, WH, GMOS, TMOS, IE, WHOS and so on, where
N is the number of reference units and
is the normalized factor.
The decision rule of Logt is as follows, where
is the variance of the distribution.
The decision rule of WH is as follows, where
i and
j are the
ith and
jth order statistic of the CRP, respectively.
The decision rule of GMOS is as follows, where
k is the kth order statistic of the CRP.
The decision rule of TMOS is as follows, where
k is the
kth order statistic of the CRP, where
and
is the cardinality of
.
The decision rule of IE is as follows:
i is the
ith order statistic of the CRP, where
and
is the cardinality of
.
The decision rule of WHOS is as follows:
i,
j, and
k are the
ith,
jth, and
kth order statistic of the CRP, respectively.
The detection capability of these incoherent CRP-CFAR detectors has been validated for various distributed clutter scenarios, but not yet for GEV clutter. Furthermore, most of these detectors are utilized as direct CFAR detectors rather than in filtering-then-CFAR detection. In the following section, the detection performance of this type of detector in the presence of filtered generalized extreme distribution clutter background is thoroughly examined.
5. Discussion
The factors that affect the performance of the filtering-then-CFAR detection scheme are the SCR enhancement capability of the adaptive filter, the level of conformity in modeling the filtered clutter distribution, and the detectability of the CFAR detector. Among the existing adaptive sea clutter filters [
11,
46,
47] that can be applied to non-coherent scanning marine radar, EVD, SVD and EMD methods have reduced suppression effects on sea clutter when dealing with the long-term accumulation process with low time resolution, resulting in unstable distribution of filtered background clutter. The efficacy of the STAF filter introduced in this paper has been validated in [
23,
24]. This paper demonstrates the stability of the filtered background clutter distribution, effectively addressing the impact of complex space-time changes in sea clutter and significantly enhancing SCR. Meanwhile, the filtered background clutter is applied to CRP-CFAR detection. Traditional CRP-CFAR, as a direct CFAR detection scheme, focuses on investigating the distribution models of original sea clutter under various sea states, wind parameters, temporal and spatial conditions, and evaluating the detection performance within these models [
20,
21,
22,
38,
39,
40]. The near and far effect and the sea spikes in the filtered background clutter distribution are markedly suppressed; however, exhibiting discernible differences from the traditional sea clutter distribution. Consequently, this paper assessed the appropriateness of seven distributions for modeling the filtered background clutter distribution and employed the GEV distribution to modeling it, presenting a novel approach for modeling the background clutter following suppression of sea clutter. Subsequently, the performance of seven CRP-CFAR detectors under GEV distribution was compared applying real data, leading to the determination of their detection capabilities. Finally, this paper adopted IE as the CFAR detector and establishes an IE CFAR detection process based on the GEV distribution.
The performance of the proposed method is excellent; however, there are still certain constraints. Firstly, several mainstream distributions are used for modeling, whereas other prevalent distributions such as the K + N, P + N, and inverse Gaussian distributions are not included. In future research, a wider range of distributions will be employed to model the filtered background clutter, and sophisticated CFAR detectors will be formulated based on these distributions.
Secondly, considering the computational demands associated with both the 3D FFT utilized in the filtering process and the GEV distribution modeling employed during detection, several optimization strategies for future research endeavors are proposed. Firstly, the 3D frequency wave-number domain adaptive filter will be reduced to a 2D framework, which not only mitigates time costs during data acquisition, but also diminishes computational complexity and resource expenditure. Secondly, by establishing a foundational GEV distribution model base and enabling rapid online matching of real-time distribution parameters, minimizing online computing resource consumption is achieved.
Thirdly, the method proposed in this paper is a filtering and detection method that leverages the stable characteristics of rough surface of sea clutter in space-time domain. This stability becomes particularly pronounced under conditions of heavy wind wave, enhancing the adaptability of our method. Conversely, in rainy environments where the rough surface of sea waves is blurred by raindrops, leading to a loss of distinctive features [
5,
48], the efficacy of the proposed method diminishes. Future research will address these rain-contaminated challenges to improve both robustness and adaptability.
Fourthly, in this paper, radar data are obtained from non-coherent scanning monopulse radar, which offers a spatial resolution of 7.5 m and a temporal resolution of 2.5 s. The proposed method demonstrates commendable performance even when relying solely on echo amplitude information, despite the low time and range resolutions. Thus, it is anticipated to outperform the radar employed in this study when applied to more advanced shipborne or airborne systems. However, the specific effectiveness requires further validation through actual data analysis. Future research will focus on assessing the generalization capability of the proposed method by incorporating a wider variety of radar types and environmental datasets.
Fifthly, the new method is different from the existing radar system and presents substantial disparities. Nevertheless, we can endeavor to address the difficulties and challenges in implementation through the following approaches. The approach in this paper adopts a modular strategy during the design process. For instance, the filtering link, the modeled link of filtered background clutter, and the CFAR detection link under the filtered background clutter distribution can all be incorporated into the radar system as independent modules. By gradually integrating into the existing systems, each module can be independently verified and optimized, minimizing the overall implementation risk and preventing the proposed approach from exerting a significant influence on the existing systems. Secondly, the method pertains to the back end processing algorithm and does not impact the signal acquisition of the radar front end. Therefore, the subsequent integration and upgrade will be more feasible when the interface between each module and the existing system can be maintained consistent. Although these approaches can alleviate the implementation difficulties to a certain extent, numerous challenges still persist, and more research is required in future work.
Finally, in this paper, a proprietary dataset is utilized. Despite the benefits of using our own dataset, it is crucial to verify the generality and robustness of the algorithm using other datasets. Therefore, in future work, conduct experimental comparisons using publicly available datasets related to our algorithm application scenarios. Meanwhile, our dataset is expanded to incorporate more data under different scenarios and conditions to further enhance the generality of the algorithm.