Beaufort Gyre westward expansion simulation using a two-layer idelized model

This data set supports the analysis presented in the manuscript: "Beta-drift of eddies drove Beaufort Gyre westward expansion during 2003-2014" (2023GL107142), which is under review for publication by Geophysical Research Letters. The model output contains 100 years of simulation for the nine models.The surface stress and deta effect are active, and their grid is configured with a 8 km horizontal resolution. 
Simulation length: 100 yearsSimulation machine: ubuntu on Desktop computerCase name: ctrl, fast moving, slow moving, large area(large tau), stress asymmetry, largeneta,smallbeta, stress-constant,f-planetTime range: 1-5182561 (corresponding to 1 to 100 model year);a model year=360 day;output frequency= 10 day

model output:
eta:sea surface height; h1:halocline layer depth;tau: surface stress;u1/v1: halocline layer horizonal velocity
The mat file is named after the corresponding case. However, it is important to note that the data names inside the mat file are not the actual case names, but rather the names used for initial records.

The model code modified from       aronnax (https://github.com/edoddridge/aronnax)
please refer to:
Doddridge, E. W., & Radul, A. (2018). Aronnax: An idealised isopycnal ocean model. Journal of Open Source Software, 3(26), 592. http://doi.org/10.21105/joss.00592
for details of this code