Disruption of Arctic Staircases by Shear: Data from Numerical Simulations

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 of Arctic Staircases by Shear,” by Brown et al., which has been submitted to the Geophysical Research Letters.

本文呈现的数值研究包含多组与北冰洋扩散对流演化相关的数值模拟。该类对流系统存在于温跃层（thermocline）中，该层的温度与盐度均随深度增加而升高。本数据集旨在作为Brown等人所撰《剪切作用对北极阶梯结构的破坏》（Disruption of Arctic Staircases by Shear）一文的补充资料，该论文已提交至《地球物理研究快报》（Geophysical Research Letters）。