Interaction of idealized urban infrastructure and long waves during run-up and on-land flow process in coastal regions

Publikation: KonferenzbeitragPaperForschungPeer-Review

Autoren

  • N. Goseberg
  • T. Schlurmann
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Details

OriginalspracheDeutsch
PublikationsstatusVeröffentlicht - 2012

Abstract

This paper reports experimental results of long wave run-up climbing up a 1:40 sloping beach. The resulting maximum run-up is compared with analytical results and a good agreement is found for single sinusoidal waves with uniform wave period and varying amplitude. Subsequently, the interaction with macro-roughness elements on the beach is investigated for different long-shore obstruction ratios. The reduction in wave run-up is expressed by means of a nomogram relating the wave run-up without macro-roughness elements present to those cases where on-land flow is modified by macro-roughness. The presented results mainly focus on a non-staggered and non-rotated macro-roughness configuration. In addition to the run-up reduction, surface elevation profiles on the shore are presented, that address the shock wave generation when the wave tongue approaches the first row of macro-roughness elements.

Schlagwörter

    Long wave, Macro-roughness, Obstruction ratio, Tsunami, Wave run-up, Beaches, Coastal engineering, Tsunamis, Long waves, Macro-roughness elements, Shock wave generation, Surface elevations, Urban infrastructure, Wave runup, Shock waves

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Interaction of idealized urban infrastructure and long waves during run-up and on-land flow process in coastal regions. / Goseberg, N.; Schlurmann, T.
2012.

Publikation: KonferenzbeitragPaperForschungPeer-Review

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AU - Goseberg, N.

AU - Schlurmann, T.

N1 - Cited By :10 Export Date: 1 February 2021

PY - 2012

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N2 - This paper reports experimental results of long wave run-up climbing up a 1:40 sloping beach. The resulting maximum run-up is compared with analytical results and a good agreement is found for single sinusoidal waves with uniform wave period and varying amplitude. Subsequently, the interaction with macro-roughness elements on the beach is investigated for different long-shore obstruction ratios. The reduction in wave run-up is expressed by means of a nomogram relating the wave run-up without macro-roughness elements present to those cases where on-land flow is modified by macro-roughness. The presented results mainly focus on a non-staggered and non-rotated macro-roughness configuration. In addition to the run-up reduction, surface elevation profiles on the shore are presented, that address the shock wave generation when the wave tongue approaches the first row of macro-roughness elements.

AB - This paper reports experimental results of long wave run-up climbing up a 1:40 sloping beach. The resulting maximum run-up is compared with analytical results and a good agreement is found for single sinusoidal waves with uniform wave period and varying amplitude. Subsequently, the interaction with macro-roughness elements on the beach is investigated for different long-shore obstruction ratios. The reduction in wave run-up is expressed by means of a nomogram relating the wave run-up without macro-roughness elements present to those cases where on-land flow is modified by macro-roughness. The presented results mainly focus on a non-staggered and non-rotated macro-roughness configuration. In addition to the run-up reduction, surface elevation profiles on the shore are presented, that address the shock wave generation when the wave tongue approaches the first row of macro-roughness elements.

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KW - Obstruction ratio

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KW - Wave run-up

KW - Beaches

KW - Coastal engineering

KW - Tsunamis

KW - Long waves

KW - Macro-roughness elements

KW - Shock wave generation

KW - Surface elevations

KW - Urban infrastructure

KW - Wave runup

KW - Shock waves

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