Citation: | WANG Zhenxi, LIANG Yongqi, GAO Pan, QIAN Na, ZHOU Liping. Ocean data visualization software (ODV and JOA) and new applications in marine geochemical studies[J]. Marine Geology Frontiers, 2024, 40(9): 96-108. doi: 10.16028/j.1009-2722.2022.032 |
Climate and biogeochemical cycle are important issues in marine sciences research fields, and the demand for fully utilizing and deeply mining marine geochemical data is growing.The internal structure of the ocean is complex and the interaction processes are diverse. The study of the internal mechanism and biogeochemical cycle of the ocean usually requires collaborative analysis of various marine physical and chemical parameters. Therefore, ocean data visualization software becomes more and more important. At present, there are few Chinese guides on the use of ocean data visualization software. Detailed description of operation level is required. Here we outline the basic functions of two data visualization softwares: Ocean Data View (ODV) and Java OceanAtlas (JOA), and provide a detailed practical guide on the production of map, section, surface, scatter, station and waterfall for the visualization, with a comparison of the differences between the two software. We also give examples of some new applications of ODV within the broad field of marine geochemistry.
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ODV data visualization operation procedures and relevant chapters in the User's Guide [5]
NORC581 voyage (November 2020 to January 2021) stations and GLODAP database stations by ODV
A still picture from the 3D-animation of distribution of dissolved iron in the Atlantic Ocean [17]
Data visualization process of JOA [7]
The seawater CFC-12 concentration data of WOCE cross-section visualized by ODV (a) and JOA (b) respectively [9]
The seawater dissolved 230Th concentration, salinity, temperature and pressure data of eGEOTRACES cross-section visualized by ODV[6]
Visualization and comparison of Δ14C data of the GEOSECS section in the East Indian Ocean
Δ14C distribution of marine air CO2 (left) and surface seawater DIC (right) in the South China Sea [22]
The intrusion depth of bomb 14C in the equatorial Eastern Indian Ocean deepens with time [23]
The changes of 14C age of modern deep sea water away from the formation area of deep water[24]
Modern and LGM Atlantic meridional (CO32–) transects [25]