Abstract

This study aims to detect a shoreline location and its changes automatically in the temporal resolution. This approach is implemented on the coastal video monitoring system applications. The proposed method applied data mining by using two main systems-a training system using classification and shoreline detection systems with Self-Organizing Map (SOM) and K-Nearest Neighbor (K-NN) algorithms. The training system performs feature texture extraction using agray-level co-occurrence matrix and the results are stored to classification process. The detection system has five processing stages: contrast stretching preprocessing and morphological contrast enhancement, SOM clustering, morphological operations, feature extraction and K-NN classification and detection shoreline. Preprocessing was used to improve the video image contrast and reliability. SOM algorithm in segmenting objects in the onshore video images. Morphological operations were applied to eliminate noise on the objects that were not needed in the spatial domain. The segmentation results of video frames classified by K-NN. The aim is to provide the class labels on each region segmentation results, namely, sea label, land label and sky label. The determination of the shoreline is done by scanning the neighboring pixels from the edge of land class label after binary image transformation. The shoreline change detection was performed by comparing the position of existing shoreline and shoreline position in the reference video frame. A Receiver Operating Characteristic (ROC) curve was used to evaluate the performance of shoreline detection systems. The results showed that the combination of SOM and K-NN was able to detect shoreline and its changes accurately.

Highlights

  • Shoreline, the contact zone between ocean and land, has changed over time due to the cross-shore movement of sediments along the shore and the dynamic nature of the water surface

  • This scheme can provide essential information concerning the shoreline in temporal resolution but it has limitations in spatial resolution

  • The video frame of the Egmondshore area was an input that was processed in the system so that the position shoreline could be shown automatically

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Summary

Introduction

The contact zone between ocean and land, has changed over time due to the cross-shore movement of sediments along the shore and the dynamic nature of the water surface. Shoreline studies have been based on field measurements of waves, currents, sediment transport and morphological changes. This scheme can provide essential information concerning the shoreline in temporal resolution but it has limitations in spatial resolution. Some logistical difficulties, such as high cost and difficulty of the survey when the weather conditions are bad, exist in this scheme (Rijn, 2007) Another method is remote sensing by using satellites or aircraft fitted with remote-sensing systems with active and passive sensors to describe the dynamics of the nearshore area. This method offers a good spatial-temporal resolution, but these observations are relatively expensive and the visibility is not extensive

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