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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">hydrophysics</journal-id><journal-title-group><journal-title xml:lang="ru">Фундаментальная и прикладная гидрофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Fundamental and Applied Hydrophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2073-6673</issn><issn pub-type="epub">2782-5221</issn><publisher><publisher-name>St. Petersburg Research Center of the Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-1135</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>ГИДРОФИЗИЧЕСКИЕ И БИОГЕОХИМИЧЕСКИЕ ПОЛЯ И ПРОЦЕССЫ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>HYDROPHYSICAL AND BIOGEOCHEMICAL FIELDS AND PROCESSES</subject></subj-group></article-categories><title-group><article-title>Изменения теплосодержания Мирового океана в период 1955–2009 гг.</article-title><trans-title-group xml:lang="en"><trans-title>Changes of Ocean Heat Content 1955–2009</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Глок</surname><given-names>Н. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Glok</surname><given-names>N. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><email xlink:type="simple">glok.natasha@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Малинин</surname><given-names>В. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Malinin</surname><given-names>V. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Российский государственный гидрометеорологический университет</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2013</year></pub-date><pub-date pub-type="epub"><day>29</day><month>11</month><year>2022</year></pub-date><volume>6</volume><issue>1</issue><fpage>32</fpage><lpage>39</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Глок Н.И., Малинин В.Н., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Глок Н.И., Малинин В.Н.</copyright-holder><copyright-holder xml:lang="en">Glok N.I., Malinin V.N.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://hydrophysics.spbrc.ru/jour/article/view/1135">https://hydrophysics.spbrc.ru/jour/article/view/1135</self-uri><abstract><p>Обсуждается межгодовая изменчивость теплосодержания Мирового океана (ТМО) с середины XX столетия по настоящее время с использованием данных разных авторов. Средний тренд ТМО составляет 0.22·1022 Дж/год и описывает 75 % дисперсии исходного ряда. С помощью вейвлет-разложения на всем рассматриваемом временнóм интервале было выявлено мощное колебание с периодом 23 года. По данным реанализа и спутников о поверхностной температуре океана построены статистические модели, с высокой точностью описывающие изменения ТМО. Показано, что начиная с 2003 г. отмечается определенная стабилизация в колебаниях ТМО.</p></abstract><trans-abstract xml:lang="en"><p>We discuss the interannual variability of the ocean heat content (OHC) from the mid-20th century to the present, using the data of different authors. An average trend of OHC is 0.22·1022 J/year, which covers 75 % variance of the source time series. A strong oscillation with the period of 23 years was detected using the wavelet analysis throughout the whole time interval under consideration. On the basis of reanalysis and the satellite sea surface temperature the statistical models accurately describing OHC changes, were designed. It is shown that since 2003 there is a certain stabilization in the variability of OHC.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>теплосодержание Мирового океана</kwd><kwd>тренд</kwd><kwd>вейвлет-анализ</kwd><kwd>статистическая модель</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в Российском государственном гидрометеорологическом университете в рамках гранта Правительства РФ (договор №11.G34.31.0078) для поддержки исследований под руководством ведущих ученых.</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Levitus S., Antonov J.I., Boyer T.P. Warming of the world ocean, 1955–2003 // Geophys. Res. let. 2005. V.32. 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