CoCoMANS Ocean App [Slides]

Abstract

Thermohaline circulation is that part of ocean circulation which is driven by density gradients. It is widely believed that changes in the ocean thermohaline circulation on the 10 to 100 year time scale can instigate rapid climate change. Scientists world wide are currently using simulation tools based on semi-implicit and split methods that are first-order in time. From a numerical error perspective, the quality of such simulations is suspect. As a result of numerical stability issues resulting from semi-implicit and split methods they are forced to use low resolution grids; ie high resolution grids will require prohibitive numbers of timesteps. Having the ability to perform such simulation with reduced splitting errors, using high resolution grids, and using second-order accurate time integration methods will be a quantum leap forward in predictive ocean simulation.