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BibEntryCargo > Journal: Acta Oceanologica Sinica & Note : Auto downloaded ref at: 2020-06-27 or Auto downloaded ref at: 2024-08-30

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A numerical simulation of latent heating within Typhoon Molave (1) · An investigation of the morphodynamic change of reef islands under monochromatic waves (1) · Assimilating satellite SST/SSH and in-situ T/S profiles with the Localized Weighted Ensemble Kalman Filter (1) · Contributions of shortwave radiation to the formation of temperature inversions in the Bay of Bengal and eastern equatorial Indian Ocean: A modeling approach (1) · Definition of water exchange zone between the Bohai Sea and Yellow Sea and the effect of winter gale on it (1) · Down-scaled regional ocean modeling system (ROMS) for high-resolution coastal hydrodynamics in Korea (1) · Effect of Langmuir circulation on upper ocean mixing in the South China Sea (1) · Identifying the sensitive areas in targeted observation for predicting the Kuroshio large meander path in a regional ocean model (1) · Improvement and application of a saturation based wave dissipation function in SWAN model (1) · Nourishment and disaster mitigation efficiency of feeding sand on the dry section of a dissipative beach (1) · Numerical investigation of wave propagation in the Liverpool Bay, NW England (1) · Numerical study of three-dimensional wave-induced longshore current’s effects on sediment spreading of the Huanghe River mouth (1) · Recent improvements to the physical model of the Bohai Sea, the Yellow Sea and the East China Sea Operational Oceanography Forecasting System (1) · Simulation of three-dimensional cohesive sediment transport in Hangzhou Bay, China (1) · Some progress on ocean data assimilation in China: Introduction of the special section “Ocean Data Assimilation” (1) · The effect of wave-induced radiation stress on storm surge during Typhoon Saomai (2006) (1) · Three-dimensional characteristics of mesoscale eddies simulated by a regional model in the northwestern Pacific Ocean during 2000–2008 (1) · Wave prediction in a port using a fully nonlinear Boussinesq wave model (1)
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