CONSIDERATION OF THE EMPIRICAL STATISTICS OF MARINE WATERS IN THE CALCULATIONS OF HYDROLOGICAL FIELDS CLIMATIC CHANGES IN THE SURFACE LAYER OF THE BLACK SEA
Based on the results of the analysis of climate histograms of joint probability density functions of seawater temperature T and salinity S, coupled with the analysis of the climate array of T-S diagrams, a statistical description of marine water masses and their properties is given, complementing the definition of these marine waters structures introduced by S.D. Dobrovolsky (1961). A relation is found between the presence of several water masses in the areas of marine research and the multimodality of joint statistical distributions of the marine waters temperature T and salinity S fields. It is shown that the neglect of climate variability of water mass statistics in the calculations of surface water temperature in the Black sea led to a lack of response to Global climate warming, noted in the results of other independent empirical studies of the sea surface in this region. Taking into account the climate changes in marine water statistics, the response to Global warming in the surface layer of the Black Sea is identified in the studied fields.