泰国湾沿岸海洋模拟:以有限体积沿岸海洋模型为例

S. Tomkratoke, S. Sirisup
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引用次数: 3

摘要

巽他大陆架位于东南亚,在那里形成了亚洲大陆大陆架的一个巨大的水下延伸。巽他大陆架包括婆罗洲、爪哇岛和苏门答腊岛的大巽他群岛,大部分大陆架形成了南中国海的浅海底,柬埔寨、马来西亚半岛、新加坡、婆罗洲的沿海地区,以及印度尼西亚、泰国和越南的部分海岸。该陆架具有复杂的海岸线和海底地形,从而导致了复杂的潮汐特征。在这项工作中,我们的目标是对该地区潮汐波的传播机制有更深刻的认识。为了实现这一点,我们对泰国湾和附近地区进行了高保真度的模拟。高保真度包括高分辨率测深(30秒)、更精细的尺度捕捉和保留真实、复杂的海岸线和岛屿的能力。为此,我们在模拟中采用有限体积法,因为它具有几何灵活性,计算效率以及体积和质量守恒保证。本文主要研究巽他陆架地区的潮汐动力过程,并对南海巽他陆架的两相系统及其对应的主潮(M2、K1、S2和O1)的能量通量进行了数值研究。与其他数值和实验观测结果进行了比较
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Coastal ocean simulation of the Gulf of Thailand: A case study of finite volume coastal ocean model
The Sunda Shelf is settled in Southeast Asia where it forms a large submerged extension of the continental shelf of mainland Asia. The Sunda shelf includes the Greater Sunda Islands of Borneo, Java and Sumatra and the bulk of the shelf forms the shallow seabed of the South China Sea, the coastal areas of Cambodia, Malaysia Peninsula, Singapore, Borneo, and parts of the coast of Indonesia, Thailand, and Vietnam. This shelf is characterized by complex shoreline and seafloor topography which can result in complicated tidal characteristics. In this work, we aim to gain insightful understanding of mechanism of the tidal wave propagation in this region. To achieve this, we perform simulation with high fidelity for the Gulf of Thailand and nearby areas. The high fidelity includes high resolution bathymetry (30 seconds), finer scale capturing and ability to preserve the realistic, complex coastline and islands. To this end, we employ the finite volume method in our simulation for its geometric flexibility, computational efficiency as well as volume and mass conservation assurance. In the current study, we focus mainly on the tidal dynamic processes in the Sunda shelf region, and we numerically scrutinize exact amphidromic systems as well as the corresponding energy flux of the principal tides (M2, K1, S2 and O1) in the Sunda shelf of the South China Sea. Comparisons to other numerical and experimental observations have been done
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