Abstract

Sandy beaches play a key role in regional tourism. It is important to understand the principal morphological processes behind preserving attractive beaches. In this study, morphological variation on the Chirihama Coast, Japan, an important local tourism resource, was investigated using two sets of field surveys. The objective was to analyze and document the multi-scale behaviors of the beach. First, long-term shoreline changes were examined based on shoreline surveys over the last two decades. Then, the middle-term behavior of multiple bar systems was analyzed based on the cross-shore profile surveys from 1998 to 2010. An empirical orthogonal function (EOF) analysis was conducted to capture the principal modes of the systematic bar migration. The shoreline analysis indicated a long-term eroding trend and showed that the seasonal variation has recently tended to increase. The profile analysis demonstrated that net offshore migrations of bars have been repeated with a return period of approximately four years. This general behavior of the bar system is similar to the net offshore migration phenomena observed at other sites in the world. EOF analysis revealed a relationship between bar configuration and middle-term variations in shoreline location; when a new bar is generated near the shoreline and a triple bar configuration is established, the shoreline tends to temporarily retreat, whereas the shoreline experiences an advance when the outer bar has most evolved.

Highlights

  • Many of the sandy beaches in the world have played an important role in regional tourism

  • Representative morphological changes on the Chirihama Coast of Japan have been investigated based on two sets of field survey records

  • The principal modes of sandbar migration obtained by empirical orthogonal function (EOF) analysis clearly captured the main features of the systematic bar behavior

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Summary

Introduction

Many of the sandy beaches in the world have played an important role in regional tourism. The long sandy beaches consist of very fine sand and are accessed by the 7 km-long ‘Nagisa Driveway’, a marine drive for automobiles on the backshore (Figure 2). More than 800,000 tourists visit the coast every year, mainly from spring to autumn, and enjoy driving automobiles on the beach. To maintain this attractive tourism resource, it is necessary to preserve the wide sandy beaches. The long sandy beach developed in this area as a segment within a large littoral cell stretching approximately 75 km along the Japan Sea coast. The principal source of sediment here is the Tedori River, the mouth of which is located approximately 45 km southwest of the study area. The sediment discharge from the Tedori River has decreased because of various anthropogenic

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