The seasonal changes in the position of the upper boundary of the Black Sea hydrogen sulfide zone due to the nature of the dynamic processes development

The position and seasonal fluctuations of the depth of the maximum water salinity gradient in the Black Sea in the upper 150 m layer (halocline), which is interpreted as the upper boundary of the hydrogen sulfide layer in the sea, were estimated based on the analysis of climatic data of the vertica...

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Bibliographic Details
Main Authors: Р.Р. Белевич, О.Р. Андріанова, М.І. Скіпа
Format: Article
Language:English
Published: Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine 2022-04-01
Series:Геофизический журнал
Subjects:
Online Access:https://journals.uran.ua/geofizicheskiy/article/view/253716
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