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Modeling of ocean overflows using statically and dynamically adaptive vertical discretization techniques

Subject Area Oceanography
Term from 2012 to 2019
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 213809913
 
Final Report Year 2020

Final Report Abstract

One of the most pressing challenges facing the current generation of the multiresolution models of regional and global ocean circulation is the preservation of water masses in long-term simulations. In this context, any significant improvement in the accuracy of numerical advection schemes and any reduction in the rate of spurious mixing for temperature and salinity can substantially enhance physical significance of models’ results and ultimately advance the predictive power of climate projections. The particular target group of our project are unstructured threedimensional ocean models which are quickly catching up with their structured counterparts in terms of model skill and computational performance. Our aim is to exploit a greater flexibility of unstructured meshes in order to reduce spurious vertical mixing. To achieve this goal we developed computationally efficient techniques that allow to adapt the vertical layer structure either statically or dynamically. The newly developed numerical methodologies were implemented in the regional ocean model UTBEST3D, they further augment model’s geometric flexibility and adaptivity features. The statically adapted meshes improve the representation of the topographically complex sea beds and could particularly benefit simulations of processes taking place near the sea floor such as sedimentation. Our technique of dynamically adapting vertical layers is fully conservative and can be used to adjust the vertical mesh structure to better fit the simulated system. An interesting application of the techniques introduced in this project could be the thermohaline circulation in the deep ocean that plays a key role in the climate system and its dynamics.

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