Numerical modeling of the sand spit elongation at Cua Lo inlet

Cua Lo Inlet is a natural tidal inlet located in the Quang Nam province in the central coastal zone of Vietnam, which is connected the Truong Giang River and An Hoa lagoon to the Gulf of Tolkin (Vietnam's East Sea). In recent years, under the influence of the winter monsoon, the updrift sand s...

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Tác giả chính: Nguyen, Quang Duc Anh
Đồng tác giả: Tanaka, Hitoshi
Định dạng: BB
Ngôn ngữ:English
Thông tin xuất bản: 2020
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Truy cập trực tuyến:http://tailieuso.tlu.edu.vn/handle/DHTL/8457
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spelling oai:localhost:DHTL-84572024-01-10T09:18:21Z Numerical modeling of the sand spit elongation at Cua Lo inlet Nguyen, Quang Duc Anh Tanaka, Hitoshi Nguyen, Trung Viet Nguyen, Xuan Tinh Sand spit River flow Winter monsoon wave Morphodynamic Inorphodynamic Computation omputation Cua Lo Inlet is a natural tidal inlet located in the Quang Nam province in the central coastal zone of Vietnam, which is connected the Truong Giang River and An Hoa lagoon to the Gulf of Tolkin (Vietnam's East Sea). In recent years, under the influence of the winter monsoon, the updrift sand spit elongation has been developed which leads to the severe deposition in the inlet. In general, when the sand spit is lengthened due to sediment accumulation on the up-drift side, breach will occur at the original location of the inlet opening to create a more efficient pathway for the water behind the sand spit (FitzGerald et al., 2001). However, due to the hydrodynamic change the breaching of sand spit in Cua Lo inlet is not incipient. This study has been investigated by the numerical models to find out the causes and the divergence of Truong Giang river flow induced by sand spit elongation under winter monsoon and river flow in flood condition influence. 2020-05-06T03:13:37Z 2020-05-06T03:13:37Z 2018 BB http://tailieuso.tlu.edu.vn/handle/DHTL/8457 en Proceedings of the 8th International Conference on Fluid Mechanics (ICFM8) September 25-28, 2018, Tohoku University, Sendai, Japan, 8 p. application/pdf
institution Trường Đại học Thủy Lợi
collection DSpace
language English
topic Sand spit
River flow
Winter monsoon wave
Morphodynamic
Inorphodynamic
Computation
omputation
spellingShingle Sand spit
River flow
Winter monsoon wave
Morphodynamic
Inorphodynamic
Computation
omputation
Nguyen, Quang Duc Anh
Numerical modeling of the sand spit elongation at Cua Lo inlet
description Cua Lo Inlet is a natural tidal inlet located in the Quang Nam province in the central coastal zone of Vietnam, which is connected the Truong Giang River and An Hoa lagoon to the Gulf of Tolkin (Vietnam's East Sea). In recent years, under the influence of the winter monsoon, the updrift sand spit elongation has been developed which leads to the severe deposition in the inlet. In general, when the sand spit is lengthened due to sediment accumulation on the up-drift side, breach will occur at the original location of the inlet opening to create a more efficient pathway for the water behind the sand spit (FitzGerald et al., 2001). However, due to the hydrodynamic change the breaching of sand spit in Cua Lo inlet is not incipient. This study has been investigated by the numerical models to find out the causes and the divergence of Truong Giang river flow induced by sand spit elongation under winter monsoon and river flow in flood condition influence.
author2 Tanaka, Hitoshi
author_facet Tanaka, Hitoshi
Nguyen, Quang Duc Anh
format BB
author Nguyen, Quang Duc Anh
author_sort Nguyen, Quang Duc Anh
title Numerical modeling of the sand spit elongation at Cua Lo inlet
title_short Numerical modeling of the sand spit elongation at Cua Lo inlet
title_full Numerical modeling of the sand spit elongation at Cua Lo inlet
title_fullStr Numerical modeling of the sand spit elongation at Cua Lo inlet
title_full_unstemmed Numerical modeling of the sand spit elongation at Cua Lo inlet
title_sort numerical modeling of the sand spit elongation at cua lo inlet
publishDate 2020
url http://tailieuso.tlu.edu.vn/handle/DHTL/8457
work_keys_str_mv AT nguyenquangducanh numericalmodelingofthesandspitelongationatcualoinlet
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