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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">mgssuvest</journal-id><journal-title-group><journal-title xml:lang="ru">Вестник МГСУ</journal-title><trans-title-group xml:lang="en"><trans-title>Vestnik MGSU</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1997-0935</issn><issn pub-type="epub">2304-6600</issn><publisher><publisher-name>Moscow State University of Civil Engineering (National Research University) (MGSU)</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.22227/1997-0935.2023.12.1957-1965</article-id><article-id custom-type="elpub" pub-id-type="custom">mgssuvest-135</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>Гидравлика. Геотехника. Гидротехническое строительство</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Hydraulics. Geotechnique. Hydrotechnical construction</subject></subj-group></article-categories><title-group><article-title>Сравнение способов определения слоя суточных осадков для расчета максимальных расходов дождевых паводков (на примере Калининградской области)</article-title><trans-title-group xml:lang="en"><trans-title>Comparison of methods for determining the layer of daily precitation for calculation of the maximum expenses of rain floods (on the example of the Kaliningrad region)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-0560-5933</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Наумов</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Naumov</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Владимир Аркадьевич Наумов — доктор технических наук, профессор, профессор кафедры техносферной безопасности и природообустройства</p><p>236022, г. Калининград, Советский пр-т, д. 1</p><p>Scopus: 16441812200, ResearcherID: T-2380-2017</p></bio><bio xml:lang="en"><p>Vladimir A. Naumov — Doctor of Technical Sciences, Professor, Professor of the Department of Technosphere Safety and Environmental Management</p><p>1 Sovetsky prospekt, Kaliningrad, 236022</p><p>Scopus: 16441812200, ResearcherID: T-2380-2017</p></bio><email xlink:type="simple">van-old@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-3483-3580</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Ахмедова</surname><given-names>Н. Р.</given-names></name><name name-style="western" xml:lang="en"><surname>Ahmedova</surname><given-names>N. R.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Наталья Равиловна Ахмедова — кандидат биологических наук, доцент, доцент кафедры техносферной безопасности и природообустройства</p><p>236022, г. Калининград, Советский пр-т, д. 1</p></bio><bio xml:lang="en"><p>Natal’ya R. Ahmedova — Candidate of Biological Sciences, Associate Professor, Associate Professor of the Department of Technosphere Safety and Environmental Management</p><p>1 Sovetsky prospekt, Kaliningrad, 236022</p></bio><email xlink:type="simple">isfendi@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Калининградский государственный технический университет (КГТУ)<country>Россия</country></aff><aff xml:lang="en">Kaliningrad State Technical University (KSTU)<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>22</day><month>12</month><year>2023</year></pub-date><volume>18</volume><issue>12</issue><fpage>1957</fpage><lpage>1965</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Наумов В.А., Ахмедова Н.Р., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Наумов В.А., Ахмедова Н.Р.</copyright-holder><copyright-holder xml:lang="en">Naumov V.A., Ahmedova N.R.</copyright-holder><license 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.vestnikmgsu.ru/jour/article/view/135">https://www.vestnikmgsu.ru/jour/article/view/135</self-uri><abstract><sec><title>Введение</title><p>Введение. Для подготовки документов территориального планирования при проектировании и строительстве следует учитывать требования организации безопасной среды жизнедеятельности, оценивать риски проявления негативного воздействия поверхностных вод, в том числе возможность затопления территории застройки. С этой целью выполняют инженерно-гидрометеорологические изыскания, определяют максимальные расчетные расходы и уровни воды в ближайших водных объектах. При проведении гидрологических расчетов важная роль отводится количественным показателям осадков, в том числе максимальным суточным осадкам. Рассмотрен способ повышения точности моделирования максимального суточного слоя ливневых осадков на примере метеостанций Калининградской области.</p></sec><sec><title>Материалы и методы</title><p>Материалы и методы. В среде MathCAD обработаны массивы данных результатов наблюдений за осадками по четырем метеостанциям: Советск (26614), Балтийск (26701), Калининград (26702), Железнодорожный (26706). Основной источник результатов наблюдений — специализированные массивы данных для климатических исследований за период 1977–2021 гг.</p></sec><sec><title>Результаты</title><p>Результаты. Определены значимая стохастическая связь между суммами годовых осадков для указанных метео-станций и слабая — между максимальными за год значениями 24-часовых сумм осадков. Рассчитаны числовые параметры рядов максимальных сумм осадков на четырех метеостанциях Калининградской области за 1977–2021 гг. Вычислено относительное превышение значений максимальных 24-часовых сумм осадков над значениями максимальных суточных сумм по метеостанциям Советск, Балтийск, Калининград, Железнодорожный.</p></sec><sec><title>Выводы</title><p>Выводы. Установлено, что с помощью 8-срочных наблюдений за осадками можно повысить точность расчета максимальных сумм суточных (24-часовых) осадков. Полученные результаты могут быть использованы при анализе осадков и расчете максимальных расходов дождевых паводков на реках с площадью водосбора менее 200 км2.</p></sec></abstract><trans-abstract xml:lang="en"><sec><title>Introduction</title><p>Introduction. To prepare territorial planning documents, during design and construction it is necessary to take into account the requirements for organizing a safe living environment, assess the risks of negative impact of surface waters, including the possibility of flooding of the development area. For this purpose, engineering and hydrometeorological surveys are carried out, the maximum estimated flow rates and water levels in the nearest water bodies are determined. When performing hydrological calculations, an important role is given to quantitative indicators of precipitation, including maximum daily precipitation. The article considers a method of increasing the accuracy of modelling the maximum daily rainfall on the example of meteorological stations in the Kaliningrad region.</p></sec><sec><title>Materials and methods</title><p>Materials and methods. Data arrays of the results of precipitation observations at four weather stations — Sovetsk (26614), Baltiysk (26701), Kaliningrad (26702), Zheleznodorozhny (26706) were processed in Mathcad. The main source of observational results is specialized datasets for climate research for the period from 1977 to 2021.</p></sec><sec><title>Results</title><p>Results. A significant stochastic relationship between the annual precipitation amounts for the indicated meteorological stations and a weak one between the maximum values of 24-hour precipitation amounts for the year were determined. Numerical parameters of the series of maximum precipitation amounts at four meteorological stations in the Kaliningrad region for 1977–2021 years are calculated. The relative excess of the values of the maximum 24-hour precipitation over the values of the maximum daily amounts at the weather stations Sovetsk, Baltiysk, Kaliningrad, Zheleznodorozhny was calculated.</p></sec><sec><title>Conclusions</title><p>Conclusions. It has been established that with the help of 8-term observations of precipitation, it is possible to increase the accuracy of calculation of the maximum amounts of daily (24-hour) precipitation. The results obtained can be used in the analysis of precipitation and calculation of the maximum discharges of rain floods on rivers with a catchment area of less than 200 km2.</p></sec></trans-abstract><kwd-group xml:lang="ru"><kwd>инженерные изыскания для строительства</kwd><kwd>максимальный расход дождевых паводков</kwd><kwd>максимальный суточный слой осадков</kwd><kwd>суточные суммы осадков</kwd><kwd>Калининградская область</kwd><kwd>статистические параметры</kwd><kwd>метеорологические сутки</kwd><kwd>гидрологические расчеты</kwd></kwd-group><kwd-group xml:lang="en"><kwd>engineering surveys for construction</kwd><kwd>maximum flow of rain floods</kwd><kwd>maximum daily precipitation layer</kwd><kwd>daily sums of precipitation</kwd><kwd>Kaliningrad region</kwd><kwd>statistical parameters</kwd><kwd>meteorological days</kwd><kwd>hydrological calculations</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Работа выполнена при финансовой поддержке Российского научного фонда и Правительства Калининградской области в рамках научного проекта № 22-27-20016.</funding-statement></funding-group><funding-group xml:lang="en"><funding-statement>The work was supported financially by the Russian Science Foundation and the Government of the Kaliningrad region within the framework of scientific project No. 22-27-20016.</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">Гельфан А.Н., Гусев Е.М., Калугин А.С., Крыленко И.Н., Мотовилов Ю.Г., Насонова О.Н. и др. 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