title: Modelling of Water Pollution Propagation in the Sevastopol Bay
abstract: Introduction. Using the original method consisting in the combined analysis of altimetry data and scanty measurements by the Argo buoys, three-dimensional fields of the temperature and salinity pseudomeasurements were previously reconstructed at the 63-500 m layer horizons, at that the areas to the right of the Rim Current and in the anticyclonic eddies up to the 125 m depth remained unfilled. Data and methods. The algorithm for restoring the unfilled areas by replenishing them with the seawater
journal: Physical Oceanography