Subset of global model sea level data for "Challenges, Advances and Opportunities in Regional Sea Level Projections: the Role of Ocean-shelf Dynamics"

Monthly sea surface height above the geoid data in NW European seas from six global simulations using the NEMO ocean model (https://www.nemo-ocean.eu/) for 1990 to 2009 ORCA0083_DFS_NWS_ssh_1990_2009, ORCA025_DFS_NWS_ssh_1990_2009, ORCA1_DFS_NWS_ssh_1990_2009, are the N006 simulation set created by Andrew Coward and the NOC Marine Systems Modelling team as used by: Baker et al 2022 Biological Carbon Pump Sequestration Efficiency in the North Atlantic: A Leaky or a Long-Term Sink? Global Biogeochemical Cycles https://doi.org/10.1029/2021GB007286, Wilson, C. et al. 2021 Significant variability of structure and predictability of Arctic Ocean surface pathways affects basinwide connectivity. Commun. Earth Environ. 2, 164. https://doi.org/10.1038/s43247-021-00237-0 (2021). These simulations are forced by the Drakkar Forcing Set 5.2 (DFS) and initialised at 1958, with a nominal 1/12, 1/4 and 1 degree resolution. See references for further model details. ORCA025_JRA_NWS_ssh_1990_2009, ORCA025_JRA_tides_NWS_ssh_1990_2009, ORCA025_JRA_ShelfPhysics_NWS_ssh_1990_2009, are new simulations produced by Chris Wilson, James Harle and the Shelf Enabled NEMO team. All are forced by the JRA reanalysis, initialised in 1976. ORCA025_JRA_NWS_ssh_1990_2009 is a reference run based on GO9, an evolution of the Joint Marine Modelling Programme configuration described by Storkey et al 2018 UK Global Ocean GO6 and GO7: a traceable hierarchy of model resolutions, Geoscientific Model Development https://gmd.copernicus.org/articles/11/3187/2018/ ORCA025_JRA_tides_NWS_ssh_1990_2009 adds explicit tides to this. ORCA025_JRA_ShelfPhysics_NWS_ssh_1990_2009 adds tides, Generic Length Scale Mixing and Multi-envelope vertical coordinates Details of these simulations can be found here: https://github.com/NOC-MSM/SE-NEMO1990年至2009年，基于NEMO海洋模型（NEMO ocean model）开展的6套全球模拟试验所得到的西北欧海域相对于大地水准面的逐月海表高度数据，模型官方网址为https://www.nemo-ocean.eu/。 ORCA0083_DFS_NWS_ssh_1990_2009、ORCA025_DFS_NWS_ssh_1990_2009、ORCA1_DFS_NWS_ssh_1990_2009属于Andrew Coward与英国国家海洋中心（NOC）海洋系统建模团队构建的N006模拟集合，该数据集已被以下研究使用： 1. Baker等人2022年发表于《全球生物地球化学循环》（Global Biogeochemical Cycles）的论文《北大西洋生物碳泵固存效率：渗漏汇还是长期汇？》，DOI: 10.1029/2021GB007286； 2. Wilson, C. 等人2021年发表于《通讯-地球与环境》（Commun. Earth Environ.）的论文《北极海洋表层路径的结构与可预测性显著变率影响盆际连通性》，卷2，第164页，DOI: 10.1038/s43247-021-00237-0 (2021)。 该系列模拟采用Drakkar强迫集5.2（Drakkar Forcing Set 5.2, DFS）进行大气强迫，初始化时间为1958年，空间分辨率分别为标称1/12度、1/4度与1度。更多模型细节可参见相关参考文献。 ORCA025_JRA_NWS_ssh_1990_2009、ORCA025_JRA_tides_NWS_ssh_1990_2009、ORCA025_JRA_ShelfPhysics_NWS_ssh_1990_2009为由Chris Wilson、James Harle与Shelf Enabled NEMO团队研发的新型模拟试验。所有试验均采用JRA再分析数据进行强迫，初始化时间为1976年。 ORCA025_JRA_NWS_ssh_1990_2009为基于GO9的参考试验，GO9是Storkey等人2018年发表于《地球科学模型开发》（Geoscientific Model Development）的论文《英国全球海洋GO6与GO7：可溯源的模型分辨率层级》所描述的联合海洋模拟计划配置的演进版本，论文网址为https://gmd.copernicus.org/articles/11/3187/2018/。 ORCA025_JRA_tides_NWS_ssh_1990_2009在此基础上加入了显式潮汐模块。 ORCA025_JRA_ShelfPhysics_NWS_ssh_1990_2009则额外加入了潮汐、通用长度尺度混合（Generic Length Scale Mixing）与多包络垂直坐标方案。 该系列模拟的详细信息可访问以下网址：https://github.com/NOC-MSM/SE-NEMO。