Estimate of significant wave height from noncoherent marine radar images by multilayer perceptrons
 3.9k Downloads
 12 Citations
Abstract
One of the most relevant parameters to characterize the severity of ocean waves is the significant wave height (H_{ s } ). The estimate of H_{ s } from remotely sensed data acquired by noncoherent Xband marine radars is a problem not completely solved nowadays. A method commonly used in the literature (standard method) uses the square root of the signaltonoise ratio (SNR) to linearly estimate H_{ s } . This method has been widely used during the last decade, but it presents some limitations, especially when swelldominated sea states are present. To overcome these limitations, a new nonlinear method incorporating additional sea state information is proposed in this article. This method is based on artificial neural networks (ANNs), specifically on multilayer perceptrons (MLPs). The information incorporated in the proposed MLPbased method is given by the wave monitoring system (WaMoS II) and concerns not only to the square root of the SNR, as in the standard method, but also to the peak wave length and mean wave period. Results for two different platforms (Ekofisk and FINO 1) placed in different locations of the North Sea are presented to analyze whether the proposed method works regardless of the sea states observed in each location or not. The obtained results empirically demonstrate how the proposed nonlinear solution outperforms the standard method regardless of the environmental conditions (platform), maintaining realtime properties.
Keywords
significant wave height marine radar multilayer perceptrons neural networks sea surface ocean waves1. Introduction
Ocean waves are oscillations of the free sea surface caused by the wind. Under severe meteorological conditions, ocean waves can be dangerous for human marine activities, such as navigation, on and offshore management, etc. One of the most important parameters to define the severity of a given ocean wave field is the socalled significant wave height, H_{ s } , which is usually defined as the average of the onethird largest wave heights of the ocean wave field of study. H_{ s } is usually estimated using insitu sensors, such as buoys, recording time series of wave elevation information. A complementary technique to analyze ocean waves is to use remote sensing imaging methods, such as coherent radars [1, 2, 3], or conventional Xband marine radars [4, 5, 6], which are noncoherent radars commonly installed in moving vessels, as well as in on and offshore platforms, or marine traffic control towers. These noncoherent radars image the sea surface at grazing incidence with horizontal polarization. Radar images are caused by the interaction of the electromagnetic fields transmitted by the radar antenna with the sea surface roughness and ripples due to the local wind [4, 7, 8]. This interaction produces a backscatter of the electromagnetic fields, which is commonly known by sailors as sea clutter, and it is an undesirable signal for navigation purposes.
The measurement of ocean waves by noncoherent Xband marine radars is based on the acquisition of temporal sequences of consecutive radar images of the sea surface. Using these data sets, the spatial and temporal variability of the sea surface is analyzed to extract an estimation of the socalled wave spectrum [4, 7, 9]. From this wave spectrum, typical sea state parameters, such us characteristic wave periods, wavelengths and wave propagation directions, can be derived to describe each sea state [6]. One of the sea state parameters commonly estimated from the wave spectrum is H_{ s } . Since noncoherent marine radars are not radiometrically calibrated, H_{ s } cannot be directly obtained from the unscaled (often logarithmically amplified as a function of range) backscatter image values. Due to the unscaled backscatter values, the wave spectral estimation is not properly scaled, and the total energy of the wave field cannot be directly estimated [9]. It is also possible to estimate H_{ s } for the case of noncoherent marine radars by using an extension of the methodology proposed for processing synthetic aperture radar (SAR) images of the sea surface [10]. This methodology is based on the estimation of the signaltonoise ratio (SNR) [9], where the signal is the spectral energy of the unscaled wave spectrum, and the noise is related to the spectral energy of the speckle noise in the radar image. Nowadays, this method is used in operational applications, being considered as a standard method for wave analysis using noncoherent Xband marine radarbased sensors in the literature.
The research study presented in this article discusses the limitations of the standard operational method used to estimate H_{ s } from marine radar image sequences. From the analysis of these limitations, the incorporation of the SNR is not enough to make accurate H_{ s } estimates in some cases (sea states). Therefore, an improved method should incorporate information from this and other sea state parameters derived from the wave spectrum. Since the wave spectrum is mainly a nonlinear process relating different wave generation sources (gravity, wind, etc.), the function implemented by the proposed method is expected to be nonlinear. Due to the inherent capabilities of artificial neural networks (ANNs) to implement nonlinear functions [11], they are investigated in this article to find a nonlinear relationship of H_{ s } with SNR and other sea state parameters. In our case of study, the multilayer perceptron (MLP), a kind of feedforward ANN, is considered. This kind of ANN is selected because it has been successfully used in the literature for different purposes when working with noncoherent marine radars. As an example, the capabilities of the MLPs to implement nonlinear functions [11] have been exploited in [12, 13] to create nonlinear filters able to reduce the sea clutter power. Moreover, due to the reduced computational cost of the MLP once designed, it can be operationally used to report H_{ s } estimates in realtime. The performances and operational properties of the proposed MLPbased method to estimate H_{ s } is studied in different sea areas, where different sea states are observed. This study will give us information about whether the MLPbased method can be applied in different sea locations or not.
The article is structured in five additional sections. Section 2 deals with the description of the radarbased system used for measuring ocean waves. This section also describes the characteristics of the insitu measurements used in this research. Section 3 introduces the standard methodology for estimating H_{ s } by using conventional noncoherent marine radar systems, including a discussion of its limitations in practical applications. Section 4 describes the new methodology proposed in the article. A description of the way an MLP is used to estimate H_{ s } , the way it is trained, its computational cost and the way the available data is divided for its design and test is given. Section 5 presents and compares the results achieved by using the standard and proposed MLPbased methodologies when estimating H_{ s } . Finally, Section 6 summarizes the main conclusions drawn from this research.
2. Instrumentation and insitu measurements
Transmission and reception characteristics of the marine radar used in the experiments
Radar system frequency (Xband)  9.5 GHz 
Antenna polarization  H and H 
Antenna rotation speed  25 rpm 
Pulse repetition frequency (PRF)  1000 Hz 
Radar pulse width  50 ns 
Azimuthal range (coverage)  0360° 
Azimuthal resolution  0.15° 
Distance range (coverage)  2004000 m 
Range resolution  7.5 m 
Two different sources of data are used in our experiments. These data were acquired in two different geographical locations of the North Sea, having different oceanographic conditions. The main properties of these platforms and their environmental characteristics are:

Ekofisk is an oil field complex, property of ConocoPhillips. Ekofisk is located in the Norwegian sector of the North Sea, about 320 km southwest of Stavanger. Typical sea state conditions in that area present severe wave fields generated by local storms. This geographical location is a wind seadominated area. In addition to these wind sea states, swelldominated wave fields can also be superimposed, having bimodal sea states. These bimodal sea states are highly dangerous for the stability of the marine structures because these structures are attacked by different wave fields propagating with different directions and different wave periods and lengths.

FINO 1 is an oceanographic research platform, being located in the German basin of the North Sea. This platform is about 45 km north of the island of Borkum. FINO 1 is operated by the Federal Maritime and Hydrographic Agency of Germany (BSH) to understand the meteorological conditions in the area to support the deployment of offshore wind farms. Although the general sea state conditions are similar to the Ekofisk area, the location of FINO 1 presents more influence of swell cases with longer wave lengths than the location of Ekofisk. In general, swell cases present longer wave lengths and wave periods than wind sea cases. In addition, swell wave fields can occur in presence of weak local wind conditions, where the roughness of the sea surface is low, and the backscattering mechanisms are weak.
3. Standard method to estimate the significant wave height from radar images of the sea surface
This section describes the basics of the method commonly used in the literature to estimate H_{ s } from marine radar images of the sea surface. This method is called "standard method" in our article. A brief description of the theoretical background of the stochastic wave theory needed to analyze ocean wave fields from marine radar data sets is presented first. The way H_{ s } is estimated by the standard method is presented after. The limitations of this method are finally discussed.
3.1. Spectral representation of ocean waves
where ω is the angular frequency, being related to the wave period T as ω = 2π/T; k = (k_{ x }, k_{ y } ) is the wave number vector, being defined by a modulus inversely proportional to the wave length λ = 2π/k, and the wave propagation direction is given by θ = tan^{1} (k_{ y } /k_{ x } ). The magnitudes dZ(k, ω) are the socalled spectral random measures, which are complex amplitudes that determine the energy of each wave component defined by the wave number and frequency (k, ω). The integration domain Ω_{k,ω}= Ω_{ k }× Ω_{ ω }is defined by the admissible range of wave lengths and periods that define the ocean waves [18] in opposition to other ocean oscillations, such as tides, planetary waves, etc. In practice, the range of wave lengths and periods that a marine radar can measure is limited by the spatial resolution of the antenna and the antenna rotation period [5]. Equation (1) indicates that the wave elevation can be regarded as a linear superposition of different individual wave components (k, ω). It is important to note that the time scale t, where both Equation (1) and the temporal sequence of radar images are defined, is shorter than the time scale of the temporal evolution of sea states, which can be seen in the examples shown in Figure 2. Hence, in opposition to t, the longer time scale related to the temporal evolution of sea states is denoted in the following as n.
where d is the water depth and U = (U_{ x }, U_{ y } ) is the socalled current of encounter [4].
In practice, the estimation of F(k, ω) takes into account a discretization of the spectral domain Ω_{k, ω}due to the spatial and temporal resolution of the sensor and the size of the total spatial oceanic area of analysis, as well as the temporal duration of the measurement [4, 7]. For standard ocean and coastal engineering applications, the 3D spectrum F(k, ω) is not used, and there are more practical wave spectral representations defined for lower spectral domain dimensions than Ω_{k, ω}. In this study, two different spectral representations are used, being [7]:
 Wave number spectrum:$\stackrel{\u0304}{F}\left(\mathbf{k}\right)=\underset{{\Omega}_{\omega}}{\int}F\left(\mathbf{k},\omega \right)d\omega .$(5)
From the spectrum $\stackrel{\u0304}{F}\left(\mathbf{k}\right)$, an important parameter derived for wave analysis is the wave number k_{ p }, where $\stackrel{\u0304}{F}\left({\mathbf{k}}_{p}\right)$ is maximum (e.g., the wave number vector related to the dominant wave component). This parameter is called peak wave number, and it defines a more relevant parameter known as peak wave length λ_{p} = 2π/k_{ p } .
 Frequency spectrum:$S\left(\omega \right)=\underset{{\Omega}_{\mathbf{k}}}{\int}F\left(\mathbf{k},\omega \right)d{k}_{x}d{k}_{y}.$(6)
3.2. Estimation of H_{ s }using temporal sequences of radar images
where c_{0} and c_{1} are calibration constants that depend on every marine radar installation [4]. Therefore, as a part of the set up of a marine radar station to estimate H_{ s } , it is necessary to carry out a calibration campaign using an insitu sensor (e.g., a buoy) to determine these calibration constants. The tuning of these constants is made by least squares method. The term SNR in Equation (9) represents the ratio between the signal of the spectral energy of the unscaled wave spectrum ($\widehat{F}\left(\mathbf{k},\omega \right)$) obtained by the inversion modeling technique and the noise of the total spectral energy of the BGN components [9].
3.3. Limitations of the standard method to estimate H_{ s }
The H_{ s } estimation from Equation (9) provides, in general, good agreements with the results derived from insitu sensors. This is valid while there is a minimum amount of local wind to induce enough sea surface roughness and, therefore, enough radar backscatter intensity [4, 9, 23]. However, under weak local wind conditions, the BGN energy is low, giving a high value of $\sqrt{\text{SNR}}$. Therefore, there is an overestimation of H_{ s } using Equation (9). It is known that, at grazing incidence, as marine radars work, shadowing is one of the most important modulation mechanisms of the radar imagery [7, 21]. In addition, the wave slopes affect the backscatter mechanisms because they change the local angle of incidence of the electromagnetic field [16]. This mechanism is called tilt modulation. Both shadowing and tilt modulation depend on the wave heights and lengths [24]. Hence, additional parameters to the $\sqrt{\text{SNR}}$ should be considered in the H_{ s } estimation. A possible solution would be including the wind speed measured by an additional sensor, like an anemometer. Nevertheless, in some radar installations, there is no wind measurements available that could give an idea about the accuracy of the H_{ s } estimation. However, as mentioned above, there are some sea state parameters derived from the wave spectra that depend indirectly on wind conditions. So, when the wind is low, long waves with long periods are expected (e.g., swelldominated sea states). In these situations, nothing useful is observed. On the contrary, when the wind speed is high, short wave lengths and periods are observed (e.g., wind seadominated sea states). In these situations, both swell and winddominated sea clutter can also be observed.
4. Estimate of the significant wave height by multilayer perceptrons
Taking into account the results presented in Section 3 (see Figure 5), the H_{ s } estimation derived by Equation (9) should be improved to obtain a more robust estimator. This improved estimator should consider additional parameters of the wave field related to the wave length and period, which depend on the wind conditions. The solution proposed here considers not only the $\sqrt{\text{SNR}}$, as done in the standard method, but also two additional parameters related to the wave length and period, such as λ_{ p }and T_{ m } . There is no indication that H_{ s } presents a linear dependence on $\sqrt{\text{SNR}}$, λ_{ p }and T_{ m } . Therefore, and since ANNs are able to implement nonlinear functions [11, 25], a nonlinear solution of the problem based on ANNs is investigated in this article. But, when proposing a solution using ANNs, several questions arise. In our case study, we need to know before selecting a type of ANN:

What kind and how many sea state parameters we should consider as input.

What kind of ANN architecture we should select, determining the type of ANN, the activation function of the ANN neurons and the ANN size.

Once the ANN architecture is selected, which learning algorithm we should use to train it.

Finally, to design and test the proposed ANNbased solution, how the database of H_{ s }measurements should be divided to correctly train the ANN and to get the best results in a testing stage.
The following sections present the answers to these questions.
4.1. MLPbased Hs estimator: architecture, data processing, and computational cost
This section presents the proposed ANNbased H_{ s } estimator, discussing what kind and how many sea state parameters are considered, and what ANN architecture (type, activation functions and size) is selected. The way the ANN processes the data and the computational cost of the proposed solution are presented at the end of the section.
Note that n represents the time scale of the sea state temporal evolution, as depicted in Figure 2, and not the time scale (t) of the temporal sequence of the radar images. In other words, the estimates made by the ANN are given at the same time instants as the measurements given by the buoy.
where f_{ANN}() denotes the inputoutput mapping function implemented by the ANN. The ANN is designed to give outputs between 0 and 10. Note that the upper limit set for the estimated H_{ s } is greater than the maximum value of H_{ s } measured by the buoy for both platforms (see Figure 2). In this way, we try to mitigate underestimates of very high values of H_{ s } .
Once knowing the kind and number of parameters to be used in the ANNbased H_{ s } estimator, the next step consists on selecting its architecture. This selection determines how the ANN processes the observation vector, and, in consequence, the way the function of Equation (11) is implemented. As noted at the beginning of the current section, a nonlinear relationship between the selected sea state parameters and H_{ s } is investigated to make accurate H_{ s } estimates. ANNs can implement this nonlinear function. Exactly, they can be implemented by MLPs [25], a kind of feedforward ANN. MLPs are able to learn from a preclassified database of measurements [11]. In this way, they can implement a proper nonlinear function between the input space (sea state parameters space) and the output space (H_{ s } space). As an example, multilayer perceptrons (MLPs) were satisfactorily used in [12, 13] as sea clutter reduction systems when working with noncoherent marine radar image sequences. In this case, MLPs were used as nonlinear filters to adapt the filtering to the nonlinear properties of the sea clutter, i.e., they were able to implement nonlinear functions. For this reason, an MLP is considered as the type of ANN used in our experiments.
Once the ANN type is selected, its size is studied. An MLP structure with two layers (input, not computed as a layer, hidden and output layers) is selected because it is demonstrated to be enough to solve a lot of kind of problems [25]. The number of MLP inputs in the input layer corresponds to the number of sea state parameters selected for this study, i.e., three inputs, being summarized in Equation (10). The number of hidden neurons in the hidden layer is selected according to the following criteria: if a few hidden neurons are selected (4, as an example), poor performance is obtained after training; but if a lot of hidden neurons are selected (50, as an example), a high risk of overfitting the training data set exists. In this way, an intermediate number of hidden neurons should be selected. As an example, in [26], where MLPs were used to create a ship detection system, the best number of hidden neurons, considering a tradeoff between performance and computational cost, was 10. Empirical studies made during our research allow us to determine that no much better performances are obtained from 15 hidden neurons for both platforms, but a computational cost increase is observed. Therefore, 15 hidden neurons are selected. Finally, one output neuron is selected because only one output is needed in the proposed system to give an estimate of the H_{ s } . As a conclusion, the selected MLP has a structure 3/15/1.
Once set the ANN type and size, the signal processing made by the MLP for a given observation vector is presented. This signal processing is summarized in Equation (11) and is computed in two steps.
Note that this layer uses a linear activation function instead of a nonlinear function, as the hyperbolic function used in the hidden neurons. It is due to during the development of the research, saturation in the H_{ s } estimate was observed in the lower and upper limits of the hyperbolic function, which correspond to low and high values of H_{ s } . This saturation is avoided using a linear activation function.
Finally, an analysis of the computational cost of the proposed solution is given. The number of operations needed to implement the MLP are given in [27] for a general MLP structure of J/K/1. Therefore, for our particular case of study (structure 3/15/1), a total of 76 memory cells (accesses to memory), 60 twoelement sums and 60 twoelement products are needed to implement it. Unfortunately, the computational cost of the solution is greater than the one needed for implementing the solution given by the standard method (one product and one sum). Nevertheless, the computational cost of the solution is still so low that realtime is not compromised when implementing it in a standard personal computer. Execution times will be reported in Section 5.
4.2. MLPbased Hs estimator: learning algorithm
Since supervised learning algorithms work properly, one of them must be selected. In this case, the error backpropagation learning algorithm is selected to train the MLP [25]. But, to make the training faster, a modified version of this algorithm is used, which incorporates an adaptive learning rate and momentum [25]. This modified version of the learning algorithm was successfully used in [12, 13, 26, 27] for different purposes. This modified learning algorithm allows automatically updating the weights (W^{(h)} and w^{(o)}) and biases (b^{(h)} and b^{(o)}) of the MLP in each algorithm iteration in a fast and stable way. An offline actualization of the weights and biases is used for training [25]. And, in order to avoid the overfitting of the designing data set during the MLP training, an external validation [25] of the training process is also carried out. This external validation is useful to stop the training when the mean squared error evaluated for a data set not used in the adaptation of the MLP weights and biases (validation data set) is increasing for consecutive algorithm iterations. In this way, the capability of generalization of the MLP to work with data sets never processed during the training stage is maintained.
4.3. Division of the databases for designing and testing the MLPbased Hs estimator
Since a supervised learning process is used to design the MLP of the proposed solution (train with external validation), we need the measurements of H_{ s } from a reference sensor. These measurements are taken from the buoys moored in the vicinity of the two platforms under study (Ekofisk and FINO 1). The measurements made by the buoy in these platforms were presented in Figure 2. But, according to the learning process presented in the section 4.2, the data of each platform must be divided in three data sets. The first and second data sets are used in the designing stage of the standard method (tuning of the calibration constants of Equation (9)) and MLPbased H_{ s } estimators. The third data set is used in a testing stage. These data sets have different purposes, being:

Training data set (designing stage): It is used in the training process of the, in which its synaptic weights and biases are updated to minimize the mean squared error of this data set.

Validation data set (designing stage): It is used during the external validation process done in the MLP learning process. This data set allows estimating how the learning process is evolving and stopping the learning process in a suitable stage where the generalization capabilities of the MLP are maintained. So, we avoid the specialization of the MLP in the training data set.

Testing data set (testing stage): This data set is used to estimate the performance of the proposed MLPbased H_{ s }estimator once designed and working autonomously.
Next, the division of the available databases of H_{ s } measurements is discussed. Three main principles drive this division:

The first principle is based on the quantity of data that will form each data set. In this way, an equitable principle (one third) is used for the division of the database in three data sets.

The second principle establishes that the first part of the database is dedicated to the designing stage and the last part to the testing stage. It is done in this way because we want to observe how the system will work for future estimates, i.e., once it is working autonomously.

And the third principle is based on the information contained in each data set of the designing stage. In this way, and based on preliminary empirical studies done during our research, to obtain high performance MLPs once trained, it is needed that the data from the worst sea state (the highest H_{ s }) are contained in the training data set.
5. Experimental results: comparison of the standard method and MLPbased Hs estimators
This section presents the H_{ s } estimations made by the proposed MLPbased method for the two platforms (Ekofisk and FINO 1) considered in the study. They are compared with the measurements made by insitu sensors (buoy). To validate the proposed method, these results are compared with the ones obtained by the standard method. The comparisons are made in the designing and testing stages. The aim of comparing the results obtained in both stages is to realize whether the performances obtained during the designing stage are maintained for a data set never processed before (testing data set) or not. In other words, we want to know, once the MLPbased estimator is designed, how the proposed method works from a point of view of performance and time of designing/execution.
5.1. Comparison of the standard method and MLPbased Hs estimators for the Ekofisk platform
The H_{ s } estimations made by the standard and MLPbased methods considering the data of the Ekofisk platform are presented first for the designing stage, and second for the testing stage.
5.1.1. Designing stage of the MLPbased Hs estimator for the Ekofisk platform
5.1.2. Testing stage of the MLPbased Hs estimator for the Ekofisk platform
5.2. Comparison of the standard method and MLPbased Hs estimators for the FINO 1 platform
As done for the case of study of the Ekofisk platform, a study of the performances of the H_{ s } estimators based on the standard method and MLPs is made in the designing and testing stages.
5.2.1. Designing stage of the MLPbased Hs estimator for the FINO 1 platform
5.2.2. Testing stage of the MLPbased Hs estimator for the FINO 1 platform
5.3. Comparison of the standard and MLPbased Hs estimators for both platforms
Comparative of the statistics of the H_{ s } estimates made by the standard method and proposed MLPbased estimators once designed, i.e., when processing the testing data set
Ekofisk  FINO 1  

Error bias  Error SD  Corr. Coef.  Error bias  Error SD  Corr. Coef.  
Standard method  0.18 m  0.27 m  0.95  +0.02 m  0.44 m  0.89 
MLPbased method  +0.14 m  0.22 m  0.97  0.03 m  0.27 m  0.96 
Improvement    18.5%  2.1%    38.6%  7.8% 
As can be observed in Table 2, the proposed method always outperforms the standard one, regardless of the platform. Moreover, it is observed that the achieved improvement is even higher for the FINO 1 platform. But, why does it happen? As described in Section 2, this platform is located in an area of the North Sea where swelldominated sea states are commonly present. In this way, it is observed that the proposed method works better than the standard one in this kind of sea states. Finally, it is important to note that, comparing the results obtained by the proposed MLPbased method for both platforms, the performances are similar. It denotes that the proposed method presents a great robustness against sea state changes and maintains its performance regardless of the sea state conditions where the marine radar images are obtained. It is important to note that since each noncoherent Xband marine radar is calibrated in each site, obtaining different calibration parameters in each one during their calibration campaigns, different estimates of sea state parameters are made, such as the SNR parameter. So, the MLPbased estimator must be designed (tuned) for each radar site, as done for tuning the constants c_{0} and c_{1} of Equation (9) in the standard method.
Finally, the time needed for designing (training with external validation) and testing an MLP is reported for both platforms. The time values presented below are obtained implementing the designing and testing stages of the MLPbased approach in Matlab 2007a and using a standard personal computer with a 2.4 GHz Intel Core2 Duo CPU, 4 GB of DDR2 PC25300 RAM and running Linux. The measured average time values are:

Designing time of an MLP for the Ekofisk platform using the training and validation data sets of Figure 7a: ≈ 30 s in average, considering a total of ≈ 30000 measurements.

Designing time of an MLP for the FINO 1 platform using the training and validation data sets of Figure 7b: ≈ 55 s in average, considering a total of ≈ 47500 measuremensurements.

Time for processing a given measurement (vector composed of: $\sqrt{\text{SNR}}$, λ_{ p }and T_{ m }) once the MLP is designed: ≈ 100 μs in average, regardless of the platform.
From an operational point of view, the design (train) of the MLP is proposed to be performed during the calibration campaign of the radar, when the data from the buoy are available.
5.4. Influence of the dimensioning and composition of the designing data sets
In the previous sections, we observed how the proposed method based on MLPs outperform the standard method when estimating H_{ s } . For doing so, we considered large data sets for designing the MLP and high values of H_{ s } in them. But, what does it happen when neither the designing data sets are so large nor it incorporates high values of H_{ s } ? For finding an answer to this question, we reduce the number of measurements (dimensioning) considered in the designing data sets of the experiments made for each platform, and vary their composition by selecting the time instants for which the measurements do not present high values of H_{ s } .

Reduction of the number of measurements used in the designing data sets in approximately 70%: from ≈ 40000 to ≈ 12600.

Reduction of the maximum H_{ s }considered in the designing data sets in approximately 17%: from ≈ 7.8 m to ≈ 6.5 m.

Reduction of the number of measurements used in the design data sets in approximately 50%: from ≈ 47500 to ≈ 23000.

Reduction of the maximum H_{ s }considered in the designing data sets in approximately 50%: from ≈ 10.0 m to ≈ 5.0 m.
6. Conclusions
A novel method for improving the H_{ s } estimate has been presented in this article. This method is based on the use of MLPs for implementing a nonlinear function that relates the selected input parameters with H_{ s } . The parameters selected in our case study are: the square root of the signaltonoise ratio $\left(\sqrt{\text{SNR}}\right)$, the peak wave length (λ_{ p }), and the mean wave period (T_{ m } ). The WaMoS II software used in the experiments extracts the values of these parameters from temporal sequences of radar images in realtime.
After analyzing the results achieved by the MLPbased method proposed for estimating H_{ s } and comparing them with the ones achieved by the standard method, four main conclusions are drawn. The first conclusion is focused on the performance improvement achieved by the proposed method. This method is able to outperform the standard method by reducing the SD of the H_{ s } estimate error and increasing the correlation coefficient of the H_{ s } time series, while maintaining a negligible estimate error bias. The second conclusion concerns to the mitigation of the problem of overestimating H_{ s } for swelldominated sea states observed in the standard method. This mitigation is achieved regardless of the platform under study. The third one concerns to the robustness of the solution against sea state changes and platform. In this way, similar performances are achieved for different places of the North Sea (different platforms), where different sea states are commonly observed. This indicates that the performances presented here can be maintained for new data sets processed in the future for the same platforms. The last conclusion is focused on the low computational cost of the proposed method. Thus, once the MLP is trained, the time needed to make an H_{ s } estimate (≈ 100 μs in average) is much lower than the time between two consecutive H_{ s } estimates (minimum of ≈ 180 s). In consequence, the proposed MLPbased H_{ s } estimator is able to process data in realtime.
Notes
Acknowledgements
This research study had been supported by Ministerio de Ciencia e Innovación, MICINN, under project number TEC200914217. The WaMoS II and buoy data obtained at the FINO 1 Platform was kindly provided by the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschiffahrt und Hydrographie, BSH) and OceanWaveS GmbH, Germany. In addition, OceanWaveS GmbH kindly provided the data acquired at the ConocoPhillips Ekofisk oil field.
Supplementary material
References
 1.Nwogu O, Lyzenga D: Surfacewavefield estimation from coherent marine radars. IEEE Geosci Remote Sens Lett 2010, 7: 631635.CrossRefGoogle Scholar
 2.Plant W, Keller W, Hayes K, Chatham C: Measuring and modeling the nrcs of the sea for backscatter. In IEEE Int Geoscience and Remote Sensing Symp 2008. IGARSS 2008. Volume 4. Boston; 2008:6568.Google Scholar
 3.Trizna D: Comparisons of a fully coherent and coherentonreceive marine radar for measurements of wave spectra and surface currents. In IEEE Oceans. Volume 1. Sydney; 2010:14.Google Scholar
 4.Reichert K, Hessner K, Dannenberg J, Tränkmann I, Lund B: Xband radar as a tool to determine spectral and single wave properties. In Proc 5th Int Symp on Ocean Wave Measurement and Analysis, WAVES 2005. Volume 1. Madrid; 2005:19.Google Scholar
 5.Hessner K, Reichert K, Dittmer J, Borge JN, Güther H: Evaluation of wamos ii wave data. In Proc of the Waves 2001 Conference. Volume 1. San Francisco; 2001:221230.Google Scholar
 6.Izquierdo P, NietoBorge J, GuedesSoares C, SanzGonzález R, Rodríguez R: Comparison of wave spectra from nautical radar images and scalar buoy data. J Waterway Port Coastal & Ocean Eng 2005, 131: 123131. 10.1061/(ASCE)0733950X(2005)131:3(123)CrossRefGoogle Scholar
 7.NietoBorge J, Rodríguez G, Hessner K, Izqiuerdo P: Inversion of marine radar images for surface wave analysis. J Atmos Ocean Technol 2004, 21: 12911300. 10.1175/15200426(2004)021<1291:IOMRIF>2.0.CO;2CrossRefGoogle Scholar
 8.Ziemer F, Brockmann C, Vaughan R, Seemann J, Senet C: Radar survey of near shore bathymetry within the oroma project. EARSeL eProc 2004, 3: 282288.Google Scholar
 9.NietoBorge J, Hessner K, JaraboAmores P, MataMoya D: Signaltonoise ratio analysis to estimate ocean wave heights from xband marine radar image time series. IET Radar Son Nav 2008, 2: 3541. 10.1049/ietrsn:20070027CrossRefGoogle Scholar
 10.Alpers W, Hasselmann K: Spectral signal to clutter and thermal noise properties of ocean wave imaging synthetic aperture radars. Int J Rem Sens 1982, 3: 423446. 10.1080/01431168208948413CrossRefGoogle Scholar
 11.Bishop C: Neural Networks for Pattern Recognition. Oxford University Press Inc., New York; 1995.zbMATHGoogle Scholar
 12.VicenBueno R, CarrascoÁlvarez R, RosaZurera M, NietoBorge JC: Sea clutter reduction and target enhancement by neural networks in a marine radar system. Sensors 2009, 9(3):19131936. 10.3390/s90301913CrossRefGoogle Scholar
 13.VicenBueno R, CarrascoÁlvarez R, RosaZurera M, NietoBorge JC, JaraboAmores MP: Artificial neural networkbased clutter reduction systems for ship size estimation in maritime radars. EURASIP J Adv Signal Proc 2010, 2010: 115.CrossRefGoogle Scholar
 14.Young I, Rosenthal W, Ziemer F: Radar survey of near shore bathymetry within the oroma project. J Geophys Res 1985, 90: 10491059. 10.1029/JC090iC01p01049CrossRefGoogle Scholar
 15.NietoBorge J, BaqueroMartinez A, de la MataMoya D, AlvarezPerez J: Analysis of the sea clutter structure using temporal sequences of xband marine radar images. In Int Conf on Radar. Volume 1. Rome; 2008:563568.Google Scholar
 16.Plant W, Keller W, Hayes K, Chatham G: Normalized radar cross section of the sea for backscatter: 1. Mean levels. J Geophys Res 2010, 115: 1121.Google Scholar
 17.Krogstad H, Trulsen K: Interpretations and observations of ocean wave spectra. Ocean Dyn 2010, 60: 973991. 10.1007/s1023601002933CrossRefGoogle Scholar
 18.Babanin A: Breaking and Dissipation of Ocean Surface Waves. Cambridge University Press, Cambridge; 2011.CrossRefzbMATHGoogle Scholar
 19.NietoBorge J: Significant wave height estimation from nautical radar data sets. Postdoc research, GKSS Research Centre, Geesthacht; 1998.Google Scholar
 20.NietoBorge J, Hessner K, Reichert K: Estimation of the significant wave height with xband nautical radars. In Ocean Mechanic and Arctic Engineering. Volume 1. Saint Johns; 1999:18. OMAE99Google Scholar
 21.Seemann J, Ziemer F, Senet C: A method for computing calibrated ocean wave spectra from measurements with a nautical xband radar. In IEEE Conf Proc Oceans 97. Volume 2. Halifax; 1997:11481154.CrossRefGoogle Scholar
 22.Terrill E, de Paolo A: Phase resolved measurements of ocean waves using Xband radar. In ONR Workshop on Deterministic Measurement and Simulation of Ocean Waves. Volume 1. La Jolla; 2009:110.Google Scholar
 23.Reichert K, Lund B: Ground based remote sensing as a tool to measure spatial wave field variations in coastal approaches. Journal of Coastal Research 2007, 50: 427431.Google Scholar
 24.Stevens C, Poulter E, Smith M, McGregor J: Nonlinear features in waveresolving microwave radar observations of ocean waves. IEEE J Ocean Eng 2002, 24: 470480.CrossRefGoogle Scholar
 25.Haykin S: Neural Networks A Comprehensive Foundation. 2nd edition. PrenticeHall, London; 1999.zbMATHGoogle Scholar
 26.VicenBueno R, CarrascoÁlvarez R, JaraboAmores MP, NietoBorge JC, AlexandreCortizo E: Detection of ships in marine environments by square integration mode and multilayer perceptrons. IEEE Trans Instrum Meas 2011, 60(3):712724.CrossRefGoogle Scholar
 27.VicenBueno R, CarrascoÁvarez R, JaraboAmores MP, NietoBorge JC, RosaZurera M: Ship detection by different data selection templates and multilayer perceptrons from incoherent maritime radar data. IET Radar Son Nav 2011, 5(2):144154. 10.1049/ietrsn.2010.0001CrossRefGoogle Scholar
Copyright information
This article is published under license to BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Open AccessThis article is distributed under the terms of the Creative Commons Attribution 2.0 International License (https://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.