Physical Model of the Mississippi Sound and Bight from 2016-05-14 to 2016-07-14

Model output of circulation, water mass and dynamical properties (currents, temperature, salinity, and sea level) for the Mississippi Bight and Mississippi Sound region of the northern Gulf of Mexico. The model application was developed as part of the GOMRI-funded CONCORDE consortium and has been configured with 400 m spatial resolution and 24 vertical layers. Surface atmospheric forcing is from a 1 km hourly product that resolves the diurnal sea breeze, which was also developed as part of the CONCORDE consortium’s modeling component (the CONCORDE Meteorological Analysis - CMA). Observed freshwater input derived from available tide gauge stations are applied as riverine forcing, and the Naval Research Laboratory-Navy Coastal Ocean Model (NRL-NCOM) output at 1 km was used as outer boundary condition forcing. The model output provided in this dataset provides a daily resolution of physical parameters (currents, temperature, salinity, water levels) for the 2016 summer recruitment season of oysters in Mississippi Sound (2016-05-14 to 2016-07-14). Other related data are available under GRIIDC Unique Dataset Identifiers (UDIs): MS.x841.000:0008 (DOI: 10.7266/SPKQN0AT), MS.x841.000:0009 (DOI: 10.7266/2SP9XTRT), MS.x841.000:0010 (DOI: 10.7266/ZKM29VT2), MS.x841.000:0011 (DOI: 10.7266/QXZVP60A), and MS.x841.000:0013 (DOI: 10.7266/FYMFTNPP).

本数据集包含墨西哥湾北部密西西比湾及密西西比海峡区域的环流、水团及动力属性（海流、水温、盐度与海平面）的模式输出结果。该模式应用由GOMRI资助的CONCORDE联盟开发，空间分辨率设置为400米，垂直分层共计24层。地表大气强迫数据源自分辨率1公里的逐时产品，该产品可解析每日海陆风环流，其同样作为CONCORDE联盟建模模块（CONCORDE气象分析系统，即CMA）的一部分开发完成。观测获取的淡水输入数据来自现有验潮站，被用作河流强迫边界；同时采用1公里分辨率的美国海军研究实验室-海军沿岸海洋模式（Naval Research Laboratory-Navy Coastal Ocean Model, NRL-NCOM）的输出结果作为外边界强迫条件。本数据集提供的模式输出为2016年密西西比海峡牡蛎夏季繁育季（2016-05-14至2016-07-14）的物理参数（海流、水温、盐度、水位）的日分辨率数据。其他相关数据可通过GRIIDC唯一数据集标识符（UDIs）获取：MS.x841.000:0008（DOI: 10.7266/SPKQN0AT）、MS.x841.000:0009（DOI: 10.7266/2SP9XTRT）、MS.x841.000:0010（DOI: 10.7266/ZKM29VT2）、MS.x841.000:0011（DOI: 10.7266/QXZVP60A）以及MS.x841.000:0013（DOI: 10.7266/FYMFTNPP）。