Mathematical model of wave transformation over radial sand ridge field on continental shelf of South Yellow Sea

According to a deformed mild-slope equation derived by Guang-wen Hong and an enhanced numerical method, a wave refraction-diffraction nonlinear mathematical model that takes tidal level change and the high-order bathymetry factor into account has been developed. The deformed mild-slope equation is u...

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Main Authors: Yao-zhong YANG, Wei-bing FENG
Format: Article
Language:English
Published: Elsevier 2010-03-01
Series:Water Science and Engineering
Subjects:
Online Access:http://www.waterjournal.cn:8080/water/EN/abstract/abstract108.shtml
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spelling doaj-b7cbd04b11944efd998c06c1cd68b6912020-11-25T00:24:44ZengElsevierWater Science and Engineering1674-23702405-81062010-03-01313646Mathematical model of wave transformation over radial sand ridge field on continental shelf of South Yellow SeaYao-zhong YANG0Wei-bing FENG1College of Harbor, Coastal and Offshore Engineering, Hohai University, Nanjing 210098, P. R. ChinaCollege of Harbor, Coastal and Offshore Engineering, Hohai University, Nanjing 210098, P. R. ChinaAccording to a deformed mild-slope equation derived by Guang-wen Hong and an enhanced numerical method, a wave refraction-diffraction nonlinear mathematical model that takes tidal level change and the high-order bathymetry factor into account has been developed. The deformed mild-slope equation is used to eliminate the restriction of wave length on calculation steps. Using the hard disk to record data during the calculation process, the enhanced numerical method can save computer memory space to a certain extent, so that a large-scale sea area can be calculated with high-resolution grids. This model was applied to wave field integral calculation over a radial sand ridge field in the South Yellow Sea. The results demonstrate some features of the wave field: (1) the wave-height contour lines are arc-shaped near the shore; (2) waves break many times when they propagate toward the shore; (3) wave field characteristics on the northern and southern sides of Huangshayang are different; and (4) the characteristics of wave distribution match the terrain features. The application of this model in the region of the radial sand ridge field suggests that it is a feasible way to analyze wave refraction-diffraction effects under natural sea conditions.http://www.waterjournal.cn:8080/water/EN/abstract/abstract108.shtmlwave transformationmathematical modelradial sand ridge fieldSouth Yellow Sea
collection DOAJ
language English
format Article
sources DOAJ
author Yao-zhong YANG
Wei-bing FENG
spellingShingle Yao-zhong YANG
Wei-bing FENG
Mathematical model of wave transformation over radial sand ridge field on continental shelf of South Yellow Sea
Water Science and Engineering
wave transformation
mathematical model
radial sand ridge field
South Yellow Sea
author_facet Yao-zhong YANG
Wei-bing FENG
author_sort Yao-zhong YANG
title Mathematical model of wave transformation over radial sand ridge field on continental shelf of South Yellow Sea
title_short Mathematical model of wave transformation over radial sand ridge field on continental shelf of South Yellow Sea
title_full Mathematical model of wave transformation over radial sand ridge field on continental shelf of South Yellow Sea
title_fullStr Mathematical model of wave transformation over radial sand ridge field on continental shelf of South Yellow Sea
title_full_unstemmed Mathematical model of wave transformation over radial sand ridge field on continental shelf of South Yellow Sea
title_sort mathematical model of wave transformation over radial sand ridge field on continental shelf of south yellow sea
publisher Elsevier
series Water Science and Engineering
issn 1674-2370
2405-8106
publishDate 2010-03-01
description According to a deformed mild-slope equation derived by Guang-wen Hong and an enhanced numerical method, a wave refraction-diffraction nonlinear mathematical model that takes tidal level change and the high-order bathymetry factor into account has been developed. The deformed mild-slope equation is used to eliminate the restriction of wave length on calculation steps. Using the hard disk to record data during the calculation process, the enhanced numerical method can save computer memory space to a certain extent, so that a large-scale sea area can be calculated with high-resolution grids. This model was applied to wave field integral calculation over a radial sand ridge field in the South Yellow Sea. The results demonstrate some features of the wave field: (1) the wave-height contour lines are arc-shaped near the shore; (2) waves break many times when they propagate toward the shore; (3) wave field characteristics on the northern and southern sides of Huangshayang are different; and (4) the characteristics of wave distribution match the terrain features. The application of this model in the region of the radial sand ridge field suggests that it is a feasible way to analyze wave refraction-diffraction effects under natural sea conditions.
topic wave transformation
mathematical model
radial sand ridge field
South Yellow Sea
url http://www.waterjournal.cn:8080/water/EN/abstract/abstract108.shtml
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AT weibingfeng mathematicalmodelofwavetransformationoverradialsandridgefieldoncontinentalshelfofsouthyellowsea
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