Disruption and Formation of Arctic Staircases by Shear: Data from Numerical Simulations

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The numerical work presented here contains a number of simulations pertinent to the evolution of diffusive convection in the Arctic Ocean. These systems exist in the thermocline, which has temperature and salinity both increasing with depth. This repository is intended as a supplement to “Disruption and Formation of Arctic Staircases by Shear,” by Brown et al., which has been submitted to the Geophysical Research Letters.

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