Wave Overtopping Discharge for Very Gently Sloping Foreshores

The spectral wave period Tm-1,0 at the toe of sea-dikes is a crucial parameter to predict wave overtopping discharge over sea-dikes. It is known from literature that this period quickly increases when waves reach shallow foreshores; however, sometimes the assumption is made that the wave period rema...

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Main Authors: Thu-Ha Nguyen, Bas Hofland, Vu Dan Chinh, Marcel Stive
Format: Article
Language:English
Published: MDPI AG 2020-06-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/6/1695
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spelling doaj-9f304eac852c4f8d87a1ec671eceaa762020-11-25T02:51:48ZengMDPI AGWater2073-44412020-06-01121695169510.3390/w12061695Wave Overtopping Discharge for Very Gently Sloping ForeshoresThu-Ha Nguyen0Bas Hofland1Vu Dan Chinh2Marcel Stive3Faculty of Civil Engineering and Geosciences, Delft University of Technology, Stevinweg 1, 2628 CN Delft, The NetherlandsFaculty of Civil Engineering and Geosciences, Delft University of Technology, Stevinweg 1, 2628 CN Delft, The NetherlandsFaculty of Coastal and Offshore Engineering, National University of Civil Engineering, Hanoi 100000, VietnamFaculty of Civil Engineering and Geosciences, Delft University of Technology, Stevinweg 1, 2628 CN Delft, The NetherlandsThe spectral wave period Tm-1,0 at the toe of sea-dikes is a crucial parameter to predict wave overtopping discharge over sea-dikes. It is known from literature that this period quickly increases when waves reach shallow foreshores; however, sometimes the assumption is made that the wave period remains constant from offshore to near-shore, leading to an underestimation of the near-shore wave period. Several formulae have been proposed to resolve the underestimation of wave overtopping discharges for very shallow foreshores. These corrective formulations confirm the tendency of underestimating the overtopping discharges over a very gently sloping foreshore but are not validated for foreshore slopes gentler than 1:500. The “equivalent slope” method based on a recent study is inappropriate for these very gently sloping foreshores due to the breaker parameter being much smaller than seven. This study proposes an extension of the correction and finds that spectral wave periods can reach values two times those offshore.https://www.mdpi.com/2073-4441/12/6/1695SWANSWASHwave overtoppingLF wavesTm−1,0(very) shallow foreshore
collection DOAJ
language English
format Article
sources DOAJ
author Thu-Ha Nguyen
Bas Hofland
Vu Dan Chinh
Marcel Stive
spellingShingle Thu-Ha Nguyen
Bas Hofland
Vu Dan Chinh
Marcel Stive
Wave Overtopping Discharge for Very Gently Sloping Foreshores
Water
SWAN
SWASH
wave overtopping
LF waves
Tm−1,0
(very) shallow foreshore
author_facet Thu-Ha Nguyen
Bas Hofland
Vu Dan Chinh
Marcel Stive
author_sort Thu-Ha Nguyen
title Wave Overtopping Discharge for Very Gently Sloping Foreshores
title_short Wave Overtopping Discharge for Very Gently Sloping Foreshores
title_full Wave Overtopping Discharge for Very Gently Sloping Foreshores
title_fullStr Wave Overtopping Discharge for Very Gently Sloping Foreshores
title_full_unstemmed Wave Overtopping Discharge for Very Gently Sloping Foreshores
title_sort wave overtopping discharge for very gently sloping foreshores
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2020-06-01
description The spectral wave period Tm-1,0 at the toe of sea-dikes is a crucial parameter to predict wave overtopping discharge over sea-dikes. It is known from literature that this period quickly increases when waves reach shallow foreshores; however, sometimes the assumption is made that the wave period remains constant from offshore to near-shore, leading to an underestimation of the near-shore wave period. Several formulae have been proposed to resolve the underestimation of wave overtopping discharges for very shallow foreshores. These corrective formulations confirm the tendency of underestimating the overtopping discharges over a very gently sloping foreshore but are not validated for foreshore slopes gentler than 1:500. The “equivalent slope” method based on a recent study is inappropriate for these very gently sloping foreshores due to the breaker parameter being much smaller than seven. This study proposes an extension of the correction and finds that spectral wave periods can reach values two times those offshore.
topic SWAN
SWASH
wave overtopping
LF waves
Tm−1,0
(very) shallow foreshore
url https://www.mdpi.com/2073-4441/12/6/1695
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AT marcelstive waveovertoppingdischargeforverygentlyslopingforeshores
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