Sensitivity of internal-tide generation to stratification and its implication for deep overturning circulations

The data sets are used for the article "Sensitivity of internal-tide generation to stratification and its implication for deep overturning circulations" by Lüschow and von Storch, published in J. Phys. Oceanogr., 2023

### meta data
- gridarea: ga_r01.nc
- ocean depth: depto_r01.nc
- ocean basins numbers: rbek_r01.nc

### barotropic tides simulated by STORMTIDE2
- Ubart_m2_2012Jan_stormtide-ncep_remap01.nc
- Vbart_m2_2012Jan_stormtide-ncep_remap01.nc

### stratification in STORMTIDE2
- 3D: N2_2012_r01.nc
- N at bottom: N_bottom_100m_r01.nc
- N homogenized: N_homogenized_r01.nc
- N averaged over full column (including cases in which the top 100,200,300 m are left out as proxy for the mixed layer): N_full_column_skip_ML_r01.nc

### density in STORNTIDE2
- interpolated to even z-levels: Rho_interpolated_to_even_levels_ym2012.nc
- transformed to neutral density and interpolated to even z-levels: Gamma_interpolated_to_even_levels_ym2012.nc

### IT generation simulated by STORMTIDE2
- uncorrected (as in Li & vonStorch 2020) but remade to 0.1-degree by 0.1-degree grid: M2_ITG_STORMTIDE2_remap01.nc

### roughness calculated from the topography used in STORNTIDE2
roughness_topo01.nc

### misc:
- extracted from Vic et al 2019 a map of the dominant IT tide mode a each grid point(very rough): dominant_mode_VicEtal2019_STORMgrid.nc