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

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