| Project/Area Number |
11680094
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| Research Category |
Grant-in-Aid for Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
自然地理学
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| Research Institution | Osaka University |
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Principal Investigator |
SUNAMURA Tsuguo Osaka University, Graduate School of Science, Professor, 大学院・理学研究科, 教授 (00011164)
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| Co-Investigator(Kenkyū-buntansha) |
TAKEDA Ichiro Kyoto Kyoiku University, Department of Education, Professor, 教育学部, 教授 (30197298)
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| Project Period (FY) |
1999 – 2001
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| Project Status |
Completed (Fiscal Year 2001)
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| Budget Amount *help |
¥3,500,000 (Direct Cost: ¥3,500,000)
Fiscal Year 2001: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 2000: ¥2,100,000 (Direct Cost: ¥2,100,000)
Fiscal Year 1999: ¥900,000 (Direct Cost: ¥900,000)
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| Keywords | Long shore bars / Multiple bars / Spilling breakers / Surf zone / Breaking waves / Large-scale turbulence / Backshore height / バー(沿岸砂州) / 後浜上限 / 多段バー / 波の遡上限界 / 水路実験 / バーの形成機構 / 海底勾配 |
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| Research Abstract |
The study aims to examine (1) the influence of the presence of long shore bars upon the subaerial beach morphology in Japan through field investigations, (2) the formative conditions for long shore bars on exposed beaches facing the Sea of Japan or the Pacific Ocean, and (3) the mechanism of the formation of long shore bars through a laboratory wave flume.
The result of the analysis of the field data obtained from 190 beaches showed that the landward limit of the backshore height is not only controlled by the grain size of beach sediment but also by the number of long shore bars: lower backshore is found at a beach with smaller number of bars. Dimensional analysis applied to the data from 25, exposed beaches facing the Sea of Japan or the Pacific Ocean indicated that the number of bars is expressed in terms of the breaker-type index to the 1.5th power. Bars are originated by the action of spilling breakers. The prevalence of wind waves on the Sea of Japan coast is conductive to the presence of multiple bars commonly found on the beach. The presence of one-bar beaches mostly on the Pacific coast is closely associated with the swell-dominated environment. The laboratory experiment showed that bars are formed by the action not only of oblique vortexes that are the already reported, large-scale turbulence induced by spilling breakers, but also of down bursts, a newly found, spilling-breaker induced turbulence, with the latter being stronger than the former. Thus, the down burst is found to be a crucial element in modeling for bar formation.
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