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Sediment Dynamics in the Adriatic Sea Investigated with Coupled Models

机译:用耦合模型研究亚得里亚海的泥沙动力学

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Several large research programs focused on the Adriatic Sea in winter 2002-2003, making it an ex-citing place for sediment dynamics modelers (Figure 1). Investigations of atmospheric forcing and oceanic reponse (including wave generation and propagation, water-mass formation, stratification and circulation), suspended material, bottom boundary layer dynamics, bottom sediment, and all-scale stratigraphy were performed by European and North American researchers participating in several projects. The goal of EuroSTRATAFORM researchers is to improve our ability to understand and simulate the physical processes that deliver sediment to the marine environment and generate stratigraphic signatures. Scientists involved in the Po and Apennine Sediment Transport and Accumulation (PASTA) experiment benefited from other major research programs including ACE (Adriatic Circulation Experiment), DOLCE VITA (Dynamics of Localized Currents and Eddy Variability in the Adriatic), EACE (the Croatian East Adriatic Circulation Experiment project), WISE (West Istria Experiment), and ADRICOSM (Italian nowcasting and forecasting) studies.
机译:2002-2003年冬季,一些大型研究计划集中在亚得里亚海,这使其成为沉积物动力学建模者的兴奋之地(图1)。欧洲和北美的研究人员对大气强迫和海洋响应(包括波浪的产生和传播,水质形成,分层和环流),悬浮物,底部边界层动力学,底部沉积物和全方位地层进行了调查。几个项目。 EuroSTRATAFORM研究人员的目标是提高我们理解和模拟将沉积物输送到海洋环境并产生地层特征的物理过程的能力。参与Po和亚平宁沉积物迁移和累积(PASTA)实验的科学家受益于其他主要研究计划,包括ACE(亚得里亚海循环实验),DOLCE VITA(亚得里亚海的局部电流动态和涡度变化),EACE(克罗地亚东亚得里亚海)循环实验项目),WISE(西伊斯特拉实验)和ADRICOSM(意大利临近预报和预报)研究。

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