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Wave-Tide-Surge Coupled Simulation for Typhoon Maemi

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China Ocean Engineering 2013年第2期27卷 141-158页

作者： Byung Ho Choi Byung Il Min Kyeong Ok Kim jin hee yuk Department of Civil and Environmental Engineering Sungkyunkwan University Marine Environments & Conservation Research Division Korea Institute of Ocean Science & Technology Supercomputing Center Korea Institute of Science and Technology Information

The main task of this study focuses on studying the effect of wave-current interaction on currents, storm surge and wind wave as well as effects of current induced wave refraction and current on waves by using numerical models which consider the bottom boundary layer and sea surface roughness parameter for shallow and smooth bed area around Korean Peninsula. The coupled system （unstructured-mesh SWAN wave and ADCIRC） run on the same unstructured mesh. This identical and homogeneous mesh allows the physics of wave-circulation interactions to be correctly resolved in both models. The unstructured mesh can be applied to a large domain allowing all energy from deep to shallow waters to be seamlessly followed. There is no nesting or overlapping of structured wave meshes, and no interpolation is required. In response to typhoon Maemi （2003）, all model components were validated independently, and shown to provide a faithful representation of the system＇s response to this storm. The waves and storm surge were allowed to develop on the continental shelf and interact with the complex nearshore environment. The resulting modeling system can be used extensively for prediction of the typhoon surge. The result show that it is important to incorporate the wave-current interaction effect into coastal area in the wave-tide-surge coupled model. At the same time, it should consider effects of depth-induced wave breaking, wind field, currents and sea surface elevation in prediction of waves. Specially, we found that：（1） wave radiation stress enhanced the current and surge elevation otherwise wave enhanced nonlinear bottom boundary layer decreased that, （2） wind wave was significantly controlled by sea surface roughness thus we cautiously took the experimental expression. The resulting modeling system can be used for hindcasting （prediction） the wave-tide-surge coupled environments at complex coastline, shallow water and fine sediment area like areas around Korean Peninsula.

关键词： typhoon Maemi finite element model tide-surge-wave coupling

Simulation for Water Quality Management in Inohana Lake Estuary, Japan

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Journal of Civil Engineering and Architecture 2010年第7期4卷 15-25页

作者： jin-hee yuk Shin-ichi Aoki Department of Civil and Environmental Engineering Sungkyunkwan University Suwon Gyeonggi-do 440- 746 Korea Department of Architecture and Civil Engineering Toyohashi University of Technology Toyohashi Aichi 441-8580 Japan

Projections of ocean climate for northwestern Pacific Ocean

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Acta Oceanologica Sinica 2005年第1期24卷 134-145页

作者： CHOI Byung Ho KIM Dong Hoon CHOI Young jin yuk jin hee Department of Civil and Environmental Engineering Sungkyunkwan University Suwon KoreaAbiko Research Laboratory Central Research Institute of Electric Power Industry JapanResearch Institute of Applied Mechanics Kyushu University JapanDepartment of Civil and Environmental Engineering Sungkyunkwan University Suwon Korea

The long-term adjustment processes of atmosphere and ocean in response to gradually increased atmospheric CO2 concentration have been analyzed in 70 and 140 a integrations with NCAR fully-coupled climate system model (CSM). In these experiments the CO2 concentration has been increased to double and quadruples the initial concentration, respectively. After 70 a, at the time of CO2 doubling, the model predicts surface air temperature rises by 1.2 and 1.5 K for the globe and the northwestern Pacific Ocean, respectively. The behavior of the quadrupling run is similar: each global and regional mean surface air temperatures increase by 2.8 and 3.0 K at the time of CO2 quadrupling. From the experiments, surface air temperature changes in the northwestern Pacific Ocean will be more distinctive compared with the global average, mainly due to exceptionally large wanning and sea level change near the entrance of the Kuroshio extension.

关键词： Climate model simulation global warming northwestern Pacific Ocean

Simulation of Suspended Sediment in the Yellow and East China Seas

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China Ocean Engineering 2005年第2期19卷 235-250页

作者： CHOI Byung-Ho MUN Jong-Yoon KO jin-Seok yuk jin-hee Department of Civil and Environmental Engineering Sungkyunkwan University Suwon 440-746 KoreaKorea Ocean Science and Engineering Corporation 175-9 Huam-dong Yongsan-gu Seoul 140-901 KoreaHyein Engineering and Construction Co. Ltd. 150-057 761 Shingil 7 dong Yungdungpogu Seoul KoreaDepartment of Civil and Environmental Engineering Sungkyunkwan University Suwon 440-746 Korea

Described is an initial attempt to simulate the suspended sediment dynamics relating to tidal and wave forcing during summertime in June 1980 and August 1981 for the Yellow and East China Seas continental shelf. The cohesive/non-cohesive sediment resuspension and movement generated by the interaction between current and wave are modeled by use of ECOMSED and WAM Cycle 4. Model results are compared with observations in US-China Marine Sedimentation Dynamics Program performed for 1980-81 at off the Changjiang estuary. The main features of simulations show that suspended sediment concentrations during the summer decreased markedly offshore as observed during the simulation periods. As for some discrepancies for the mouth of the estuary with high river discharges, i.e., the Changjiang River, the model did not properly reproduce the over-mixing situation in the summer; thus distinct vertical concentration variation in this local region is not agreeable with observation. However, general dispersal patterns of suspended sediment movement seem to be agreeably reproduced for the nearshore shallow region. Some of the procedures of simulation and results are presented and discussed.

关键词： Yellow Sea East China Sea sediment transport model time slice experiment sediment concentration