An ANN application for water quality forecasting
Introduction
Seawater is a primary natural resource for many coastal development sectors. It is also one of the most sensitive and vulnerable resources, because it is negatively impacted by a variety of anthropogenic activities. Deterioration of coastal water quality has triggered the initiation of serious management efforts in many countries. Tourism, recreation, and fishing require at least an acceptable level of seawater quality. Singapore, an island state, has stringent enforcement and continuously upgraded waste handling facilities to guarantee seawater of a certain quality.
Most acceptable ecological and social decisions are difficult to make without careful modeling, prediction/forecasting, and analysis of seawater quality for typical development scenarios. Water quality prediction enables a manager to choose an option that satisfies a large number of identified conditions. For instance, water quality variables, such as salinity, temperature, nutrients, dissolved oxygen (DO), and chlorophyll-a (Chl-a), in coastal water describe a complex process governed by a considerable number of hydrologic, hydrodynamic, and ecological controls that operate at a wide range of spatiotemporal scales. Sources of the admixtures often cannot be clearly identified, and the locally influenced complex mass exchange between the variables may not be known. Due to the correlations and interactions between water quality variables, it is interesting to investigate whether a domain-specific mechanism governing observed patterns exists to prove the predictability of these variables. The identification of such forecast models is particularly useful for ecologists and environmentalists, since they will be able to predict seawater pollution levels and take necessary precaution measures in advance.
Classical process-based modeling approaches can provide good estimations of water quality variables, but they usually are too general to be applied directly without a lengthy data calibration process. They often require approximations of various processes, and these approximations may overlook some important factors affecting the processes in seawater. A process-based model requires a lot of input data and model parameters that are often unknown, while data-driven techniques provide an effective alternative to conventional process-based modeling. Models developed by data-driven techniques are computationally very fast and require fewer input parameters than process-based models. Data-driven modeling techniques have gained popularity in the last 20 years. The scientific and engineering communities have acquired already extensive experience in the development and usage of data-driven techniques. ANNs are, however, still not widely used tools in the fields of water quality prediction and forecasting. ANNs are able to approximate accurately complicated non-linear input–output relationships. Like their physics-based numerical model counterparts, ANNs require training or calibration. After training, each application of the trained ANN is an estimation of a simple algebraic expression with known coefficients and is executed practically instantaneously. The ANN technique is flexible enough to accommodate additional constraints that may arise in the application.
This paper demonstrates the application of ANNs to model the values of selected seawater quality variables, having the dynamic and complex processes hidden in the monitored data itself. The ANN model can reveal hidden relationships in the historical data, thus facilitating the prediction and forecasting of seawater quality. The steps followed in the development of such models include the choice of performance criteria, division and pre-processing of the available data, determination of appropriate model inputs and network architecture, optimization of the connection weights (training), and model validation. In this paper, a study of ANN modeling to predict and forecast temperature, salinity, DO, and Chl-a in Singapore coastal waters is presented. These water quality parameters were measured weekly at various locations. These models could be used as a prediction tool, which complements the process-based model and ongoing field monitoring program in the region. The results of the ANN prediction and forecast model in the East Johor Strait are discussed in this paper.
Section snippets
Study area and water quality data
Singapore is a tropical country located between latitudes 1°06′N and 1°24′N and longitudes 103°24′E and 104°24′E, 137 km north of the equator. Singapore is located in Southeast Asia at the southern tip of the Malaysian Peninsula between Malaysia and Indonesia. The coastal water of Singapore is bounded by the Johor Strait in the north and the Singapore Strait in the south. Singapore is a small island having a total land area of 699 km2, with air temperature ranging from 21.1 to 35.1 °C, and annual
Temperature model results
The ANN model was developed to simulate weekly seawater temperature in the East Johor Strait of Singapore with respect to time and space. It used an ANN architecture BP with three hidden layers with different activation functions (wardnet) and an initial weight of 0.3. The optimum learning rate of 0.1 and momentum of 0.1 were selected as explained in Section 2.2.2. The sensitivities of the above parameters for the temperature prediction are smaller for the training and test data sets than they
Summary and conclusions
ANN models were developed to predict salinity, water temperature, dissolved oxygen and Chl-a concentrations in Singapore coastal waters both temporally and spatially using continuous weekly measurements of water quality variables at different stations. In spite of largely unknown factors controlling seawater quality variation and the limited data set size, a relatively good correlation was observed between the measured and predicted values. The ANN modeling technique’s application for dynamic
Acknowledgments
The authors thank the authors A.L Chuah and K.Y.H. Gin for the published data in “Water quality study of the East Johor Strait” (1998). We also thank the Tropical Marine Science Institute for financial support and provided technical facilities.
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