Zobrazeno 1 - 10
of 38
pro vyhledávání: '"Jae-Youll Jin"'
Publikováno v:
Water, Vol 16, Iss 6, p 836 (2024)
In this study, a swash-zone model, using Larson and Wamsley formula (LW07), was combined into the Telemac-2D model system to examine the performance of modeling swash-zone processes through comparisons with field observation data. The experimental si
Externí odkaz:
https://doaj.org/article/ff2fbb5811cf40579dc8cdd520fb0e02
Autor:
Jong Dae Do, Jae-Youll Jin, Byunggil Lee, Weon Mu Jeong, Jin Yong Choi, Sang Kwon Hyun, Kihyun Kim, Yeon S. Chang
Publikováno v:
Frontiers in Marine Science, Vol 9 (2022)
Coastal erosion caused by extreme storms can reduce the value of beaches. Under the scenario of climate change, the storm intensity may increase and the resulting severe erosion can lead to disastrous damages on the beaches. Therefore, it is crucial
Externí odkaz:
https://doaj.org/article/2a63e28458d74f3d9845c1f98ca8403a
Autor:
Jong-Dae Do, Sang-Kwon Hyun, Jae-Youll Jin, Byunggil Lee, Weon-Mu Jeong, Kyong-Ho Ryu, Won-Dae Back, Jae-Ho Choi, Yeon S. Chang
Publikováno v:
Journal of Marine Science and Engineering, Vol 10, Iss 12, p 2032 (2022)
Severe shoreline erosions are commonly observed due to the side effects of breakwaters constructed to protect the habitat. These breakwaters can cause wave energy differences behind the structure due to diffraction, inducing longshore sediment transp
Externí odkaz:
https://doaj.org/article/2e662adc75a946e0aea6f25fd398a4bb
Autor:
Jae-Youll Jin, Jong Dae Do, Jin-Soon Park, Jun Seok Park, Byunggil Lee, Sung-Doo Hong, Sung-Ju Moon, Keun Choon Hwang, Yeon S. Chang
Publikováno v:
Frontiers in Marine Science, Vol 8 (2021)
The west coast of South Korea is characterized by a wide macrotidal area with a maximum tidal range of ∼10 m. The sea surface elevation varies with the tidal phase, which leads to significant changes in the vertical structure of the physical, chemi
Externí odkaz:
https://doaj.org/article/77d4e0057d0c4991b09866ecd1eae0f3
Hydrodynamic Measurements of Propagating Waves at Different Nearshore Depths in Hujeong Beach, Korea
Publikováno v:
Journal of Marine Science and Engineering, Vol 8, Iss 9, p 690 (2020)
This paper reports the results of hydrodynamic measurements at two different water depths to observe wave properties in the course of wave propagation, especially during storm periods, in Hujeong Beach, Korea. In addition to hydrodynamic measurements
Externí odkaz:
https://doaj.org/article/6a9616ddd1a8461399b1796567651ac6
Publikováno v:
Applied Sciences, Vol 9, Iss 23, p 4984 (2019)
Shoreline processes observed by a video monitoring system were investigated under different wave conditions. A 30 m-high tower equipped with video cameras was constructed in Hujeong Beach, South Korea, where coastal erosion was suspected to occur. Tw
Externí odkaz:
https://doaj.org/article/e1dc193037a84eadbf124f401c3008bd
Autor:
Jae-Youll Jin, Weonmu Jeong, Jae Ho Choi, Yeon S. Chang, Jong Dae Do, Won-Dae Baek, Sang Kwon Hyun
Publikováno v:
Ocean Science Journal. 55:1-16
Beach erosion is a serious problem that can be aggravated by human-made structures, and the modeling of breaking waves near the coast and around coastal structures can be used to determine their impact. In this study, OpenFoam was employed to simulat
Publikováno v:
Journal of Hydro-environment Research. 29:31-44
Since Gangneung Harbor breakwaters were built in the east coast of Korea from 1992 to 2002, the shoreline inside the harbor had severely changed as it was accreted in the area inside the harbor but eroded further south during the observation period (
Autor:
Sung-Ju Moon, Jun-Seok Park, Byunggil Lee, Keun Choon Hwang, Jinsoon Park, Jong Dae Do, Sung-Doo Hong, Yeon S. Chang, Jae-Youll Jin
Publikováno v:
Frontiers in Marine Science, Vol 8 (2021)
The west coast of South Korea is characterized by a wide macrotidal area with a maximum tidal range of ∼10 m. The sea surface elevation varies with the tidal phase, which leads to significant changes in the vertical structure of the physical, chemi
Publikováno v:
Geophysical Research Letters. 46:9804-9812