В качестве одного из механизмов мультидекадной изменчивости климата следует рассматривать автоколебательный процесс перераспределения тепла в системе океан-атмосфера-континент. На основе данных наблюдений (1960-2014 гг.) оценивают междекадные изменения теплосодержания верхнего деятельного слоя в северо-западной части Тихого океана, которая является одним из информативных районов Мирового океана.
The article touches upon the methodological problems of underwater investigation of the bottom fauna, plants, micro and meso-relief of the Russian Arctic in connection with the study of regional ecosystems. The methods and technical means of underwater observations used in the Arctic expeditions of the Institute of Oceanology are considered. Technical solutions that increase the effectiveness of sonar and visual inspection of the bottom surface are proposed. The results of experimental studies are given.
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