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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">aari</journal-id><journal-title-group><journal-title xml:lang="ru">Проблемы Арктики и Антарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Antarctic Research</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0555-2648</issn><issn pub-type="epub">2618-6713</issn><publisher><publisher-name>Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.30758/0555-2648-2023-69-3-272-289</article-id><article-id custom-type="elpub" pub-id-type="custom">aari-543</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>ОКЕАНОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>OCEANOLOGY</subject></subj-group></article-categories><title-group><article-title>Приливные и непериодические колебания уровня воды в средней части Обской губы</article-title><trans-title-group xml:lang="en"><trans-title>Tidal and nontidal variations in the water level in the middle part of the Ob’ Bay</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>Войнов</surname><given-names>Г. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Voinov</surname><given-names>G. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Gennadiy N. Voinov</p><p>St. Petersburg</p><p> </p></bio><email xlink:type="simple">voinovgn@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>Пискун</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Piskun</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Alexander A. Piskun</p><p>St. Petersburg</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ФГБУ Государственный океанографический институт им. Н.Н. Зубова, Санкт-Петербургское отделение; ГНЦ РФ Арктический и антарктический научно-исследовательский институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>State Oceanographic Institute, St. Petersburg Branch; State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>ГНЦ РФ Арктический и антарктический научно-исследовательский институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>02</day><month>10</month><year>2023</year></pub-date><volume>69</volume><issue>3</issue><fpage>272</fpage><lpage>289</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Войнов Г.Н., Пискун А.А., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Войнов Г.Н., Пискун А.А.</copyright-holder><copyright-holder xml:lang="en">Voinov G.N., Piskun A.A.</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://www.aaresearch.science/jour/article/view/543">https://www.aaresearch.science/jour/article/view/543</self-uri><abstract><p>Предложены новые оценки гармонических постоянных прилива на летний (август) и зимний (апрель) периоды на постах Сабетта, Утренний, на постах Тадибеяха и Сеяха, а также в пунктах м. Харсе, м. Яптик-Сале, м. Котельникова и м. Хампуль-Яха. Исследование непериодических колебаний уровня на постах Тадибеяха и Сеяха основано на однородных рядах, а также остаточных (наблюдения минус предвычисления). </p></abstract><trans-abstract xml:lang="en"><p>New estimates are suggested of harmonic constants of the tide for the summer (August) and winter (April) periods at the Sabetta, Utrenny posts, at the Tadibeyakha and Seyakha posts, as well as at the points of Cape Kharse, Cape Yaptik-Sale, Cape Kotelnikova and Cape Hampul-Yakha. The harmonic analysis of the tide was carried out using the least squares method according to the AARI version. According to AARI expedition observations in Sabetta for the period 2012–2016, and in Salman for the period 2016–2019, average vector estimates for each month of the year have been obtained. The observations were made using the ADCP device installed at autonomous buoy stations. Hourly level observations at the Seyakha and Tadibeyakha posts for the entire observation period from 1968 to 1992 were brought to a homogeneous form using the calibration method. The historical observations of the level at the points of Cape Kharse, Cape Yaptik-Sale, Cape Kotelnikova and Cape Khampul-Yakha, carried out in different years, are of scientific interest. Since the results of their processing and analysis in the original sources contained errors and did not include shallow water constituents, our analysis results are presented. Our tests show a significant contribution of shallow water constituents in the Ob’ Bay to the description of the tide curve and the calculation of the heights and times of high and low waters. Inter-annual and intra-annual estimation is given of the dispersions of the total and tidal level fluctuations in Seyakha and Tadibeyakha for the entire observation period. Comparison of the average seasonal course of the tide in the annual cycle based on the results of tide analysis in Seyakha and Tadibeyakha (XX century) and Sabetta and Utrenny (XXI century) shows significant differences. The study of surges of level is based on uniform series, as well as residual ones (observations minus predictions). </p></trans-abstract><kwd-group xml:lang="ru"><kwd>волна М2</kwd><kwd>гармонические постоянные</kwd><kwd>приливы</kwd><kwd>сезонный ход</kwd><kwd>статистические характеристики</kwd></kwd-group><kwd-group xml:lang="en"><kwd>M2 tide</kwd><kwd>harmonic constants</kwd><kwd>seasonal variation</kwd><kwd>statistical characteristics</kwd><kwd>tides</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено в рамках темы 2.2 Плана НИТР Росгидромета на 2022 г.</funding-statement><funding-statement xml:lang="en">The research was funded within project 2.2 of Roshydromet Plan NITR 2022.</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">Корт В.Г. 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