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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">10.30758/0555-2648-2020-66-4-463-481</article-id><article-id custom-type="elpub" pub-id-type="custom">aari-320</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>ФИЗИКА АТМОСФЕРЫ И ГИДРОСФЕРЫ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>ATMOSPHERE AND HYDROSPHERE PHYSICS</subject></subj-group></article-categories><title-group><article-title>Критические уровни летней межени на устьевых участках рек Обско-Тазовского региона</article-title><trans-title-group xml:lang="en"><trans-title>Critical levels of the summer season in the mouth areas of the rivers of the Ob-Taz region</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>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"/><bio xml:lang="en"><p>Alexander A. Piskun</p><p>St. Petersburg</p></bio><email xlink:type="simple">piskun@aari.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><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>2020</year></pub-date><pub-date pub-type="epub"><day>28</day><month>11</month><year>2020</year></pub-date><volume>66</volume><issue>4</issue><fpage>463</fpage><lpage>481</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Пискун А.А., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Пискун А.А.</copyright-holder><copyright-holder xml:lang="en">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/320">https://www.aaresearch.science/jour/article/view/320</self-uri><abstract><p>Выполнены анализ продолжительности стояния уровня воды ниже проектных отметок и оценка его характеристик за навигационный период на постах Салехард, Аксарка, Ныда, Надым, Самбург, Сидоровск, Тазовский, Находка на рядах наблюдений по 2013 г. Выделены случаи непрерывного стояния уровней не менее 10 суток, что относится к опасным явлениям. В результате анализа получены оценки продолжительности и повторяемости непрерывного стояния уровней в периоды открытого русла за каждый год, за 10-летние интервалы, за многолетие. Определены соотношения частоты и продолжительности опасных случаев с продолжительностью навигационных периодов. Установлены превышения критических уровней над минимальными за периоды наиболее продолжительных случаев непрерывного стояния за сезон открытого русла. Выполнено сравнение суммарной за сезон продолжительности стояния уровней ниже проектных значений с характеристиками стока воды для постов при наличии необходимой информации.</p></abstract><trans-abstract xml:lang="en"><p>Situations in which water levels in summer fall below design (critical) marks for at least 10 days are considered dangerous phenomena. In such situations, navigation is hampered or stopped, resulting in significant economic damage. As our previous studies have shown, the mouth areas of the rivers of the Ob-Taz region that are used for navigation are prone to these dangerous phenomena. The aim of this work is to analyze the duration of the water level standing below the design marks and to estimate its characteristics for the navigation period at the posts Salekhard, Aksarka, Nyda, Nadym, Samburg, Sidorovsk, Tasovsky, Nahodka over an extended series of observations. Of the posts listed, the analysis has not previously covered Aksarka and Nadym data. Project levels have changed for some of the posts over the years, requiring updated estimates. The analysis was carried out on the basis of average daily levels at the posts for the period 1936-2013 published in the annual edition of the Water cadastre. If necessary, information on the water flow was included. Unfortunately, the quality of the data for most of the posts except Salekhard is not satisfactory due to numerous passes. The technique consists in the analysis of continuous level standing relative to the design values by specified intervals of duration. The results show that all the posts experienced levels lower than the design marks. In Nahodka it happened annually, in Nadym, Samburg, Sidorovsk — in 75.6 %, 68.3 %, 54.2 % of all the years of observations, respectively. Of all the cases of standing levels below the design mark, those of continuous standing with a dangerous duration were observed in Sidorovsk 71 %, Nadym 67.3 %, Samburg 41.1 %, Nahodka 40.0 %, Aksarka 26.1 %, Nyda 19.1 %, Salekhard 16.7 %. Only in Tasovsky were there no cases of dangerous duration. The largest number of years with dangerous cases fall on the 10-th anniversary of 1981-1990. In individual navigation seasons, two to four cases of continuous standing levels of dangerous duration were observed. At the same time, minimum average daily levels fell below critical values by a value from 189 cm (Nahodka) to 53 cm (Samburg). The maximum number of days with cases of dangerous duration in one season was in shares from the period of open channel from 91.4 % (Nahodka) to 36.6 % (Salekhard). The sum of days with levels below the design values for the season depends inversely on the amount of river flow.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>навигационные периоды</kwd><kwd>опасные явления</kwd><kwd>повторяемость</kwd><kwd>продолжительность</kwd><kwd>проектные отметки</kwd><kwd>характеристики</kwd></kwd-group><kwd-group xml:lang="en"><kwd>characteristics</kwd><kwd>design marks</kwd><kwd>duration</kwd><kwd>hazards</kwd><kwd>navigation periods</kwd><kwd>repeatability</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено при финансовой поддержке РФФИ в рамках научного проекта № 18-05-60192</funding-statement><funding-statement xml:lang="en">The reported study was funded by RFBR, project number 18-05-60192</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">Руководящий документ. Инструкция. 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