Numerical study of coastal wave profiles at the sandy beaches of Nowshahr (Southern Caspian Sea)

This study aimed to investigate the capability of the one-dimensional (1D) mode of the Simulating WAves till SHore (SWASH), as a non-hydrostatic wave-flow model with six vertical layers, to reproduce the cross-shore wave evolution. For this purpose, the given model was initially calibrated for wave...

Full description

Saved in:
Bibliographic Details
Main Authors: Seyed Masoud Mahmoudof, Mohammadali Lotfi Takami
Format: Article
Language:English
Published: Institute of Oceanology of the Polish Academy of Sciences 2022-07-01
Series:Oceanologia
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S0078323422000252
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1849324946847694848
author Seyed Masoud Mahmoudof
Mohammadali Lotfi Takami
author_facet Seyed Masoud Mahmoudof
Mohammadali Lotfi Takami
author_sort Seyed Masoud Mahmoudof
collection DOAJ
description This study aimed to investigate the capability of the one-dimensional (1D) mode of the Simulating WAves till SHore (SWASH), as a non-hydrostatic wave-flow model with six vertical layers, to reproduce the cross-shore wave evolution. For this purpose, the given model was initially calibrated for wave energy and the outputs were then verified with the field data measured at the Southern Caspian Sea. The calibration coefficients obtained for wave breaking are significantly less than the ones which have been mostly reported in previous studies for the two-dimensional (2D) mode of the SWASH. Although the reproduced wave height parameters are generally in good accordance with the field observations, the period parameters and the number of waves are overestimated and underestimated by the model, respectively. Moreover, the inaccuracies at the shallow stations are worse than at the transitional depths. The overestimation in both the reproduced energy of infragravity waves (IG) and their wavelength along with the underestimation in the wind-wave energy content are also among the factors responsible for the model deficiencies. The findings have revealed that the overestimation of the reproduced IG waves is the main reason for the underestimation of the breaking dissipation rate for irregular wave trains in the 1D mode. Therefore, more intensive breaking dissipation via selecting lower coefficient values is necessary to exhaust a certain energy content from longer waves in the 1D mode. This approach ultimately induces an over-dissipation of short wind-waves.
format Article
id doaj-art-7bc5bb24cbc8485582941270d060e979
institution Kabale University
issn 0078-3234
language English
publishDate 2022-07-01
publisher Institute of Oceanology of the Polish Academy of Sciences
record_format Article
series Oceanologia
spelling doaj-art-7bc5bb24cbc8485582941270d060e9792025-08-20T03:48:32ZengInstitute of Oceanology of the Polish Academy of SciencesOceanologia0078-32342022-07-0164345747210.1016/j.oceano.2022.03.001Numerical study of coastal wave profiles at the sandy beaches of Nowshahr (Southern Caspian Sea)Seyed Masoud Mahmoudof0Mohammadali Lotfi Takami1Corresponding author at: Iranian National Institute for Oceanography and Atmospheric Sciences (INIOAS), Tehran, 1411813389, Iran.; Iranian National Institute for Oceanography and Atmospheric Sciences (INIOAS), Tehran, IranIranian National Institute for Oceanography and Atmospheric Sciences (INIOAS), Tehran, IranThis study aimed to investigate the capability of the one-dimensional (1D) mode of the Simulating WAves till SHore (SWASH), as a non-hydrostatic wave-flow model with six vertical layers, to reproduce the cross-shore wave evolution. For this purpose, the given model was initially calibrated for wave energy and the outputs were then verified with the field data measured at the Southern Caspian Sea. The calibration coefficients obtained for wave breaking are significantly less than the ones which have been mostly reported in previous studies for the two-dimensional (2D) mode of the SWASH. Although the reproduced wave height parameters are generally in good accordance with the field observations, the period parameters and the number of waves are overestimated and underestimated by the model, respectively. Moreover, the inaccuracies at the shallow stations are worse than at the transitional depths. The overestimation in both the reproduced energy of infragravity waves (IG) and their wavelength along with the underestimation in the wind-wave energy content are also among the factors responsible for the model deficiencies. The findings have revealed that the overestimation of the reproduced IG waves is the main reason for the underestimation of the breaking dissipation rate for irregular wave trains in the 1D mode. Therefore, more intensive breaking dissipation via selecting lower coefficient values is necessary to exhaust a certain energy content from longer waves in the 1D mode. This approach ultimately induces an over-dissipation of short wind-waves.http://www.sciencedirect.com/science/article/pii/S0078323422000252SWASH ModelCaspian SeaWave evolutionInfragravity wavesShort wind-waves
spellingShingle Seyed Masoud Mahmoudof
Mohammadali Lotfi Takami
Numerical study of coastal wave profiles at the sandy beaches of Nowshahr (Southern Caspian Sea)
Oceanologia
SWASH Model
Caspian Sea
Wave evolution
Infragravity waves
Short wind-waves
title Numerical study of coastal wave profiles at the sandy beaches of Nowshahr (Southern Caspian Sea)
title_full Numerical study of coastal wave profiles at the sandy beaches of Nowshahr (Southern Caspian Sea)
title_fullStr Numerical study of coastal wave profiles at the sandy beaches of Nowshahr (Southern Caspian Sea)
title_full_unstemmed Numerical study of coastal wave profiles at the sandy beaches of Nowshahr (Southern Caspian Sea)
title_short Numerical study of coastal wave profiles at the sandy beaches of Nowshahr (Southern Caspian Sea)
title_sort numerical study of coastal wave profiles at the sandy beaches of nowshahr southern caspian sea
topic SWASH Model
Caspian Sea
Wave evolution
Infragravity waves
Short wind-waves
url http://www.sciencedirect.com/science/article/pii/S0078323422000252
work_keys_str_mv AT seyedmasoudmahmoudof numericalstudyofcoastalwaveprofilesatthesandybeachesofnowshahrsoutherncaspiansea
AT mohammadalilotfitakami numericalstudyofcoastalwaveprofilesatthesandybeachesofnowshahrsoutherncaspiansea