Sensitivity of internal-tide generation to stratification and its implication for deep overturning circulations
收藏doi.org2023-11-20 更新2025-03-24 收录
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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
该数据集被应用于Lüschow与von Storch所著，发表于《海洋物理学报》（J. Phys. Oceanogr.）2023年的文章《内部潮汐生成对层结的敏感性及其对深层翻转环流的启示》。### 元数据 - 网格区域：ga_r01.nc - 海洋深度：depto_r01.nc - 海洋盆地数量：rbek_r01.nc ### 由STORMTIDE2模拟的潮汐：- 水平潮：Ubart_m2_2012Jan_stormtide-ncep_remap01.nc - 垂直潮：Vbart_m2_2012Jan_stormtide-ncep_remap01.nc ### STORMTIDE2中的层结信息 - 3D：N2_2012_r01.nc - 底部N：N_bottom_100m_r01.nc - 均质化N：N_homogenized_r01.nc - 对整个柱状平均的N（包括顶部100、200、300米作为混合层的替代）：N_full_column_skip_ML_r01.nc ### STORMTIDE2中的密度信息 - 插值到均匀的z级面上：Rho_interpolated_to_even_levels_ym2012.nc - 转换为中性密度并插值到均匀的z级面上：Gamma_interpolated_to_even_levels_ym2012.nc ### 由STORMTIDE2模拟的内部潮生成 - 未校正（如Li & vonStorch 2020中所述）但重新制作成0.1度×0.1度网格：M2_ITG_STORMTIDE2_remap01.nc ### 由STORMTIDE2使用的地形计算的粗糙度：roughness_topo01.nc ### 其他：- 从Vic等（2019年）提取，每个网格点的主导内部潮汐模式图（非常粗糙）：dominant_mode_VicEtal2019_STORMgrid.nc
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