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<article 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" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Ice and Snow</journal-id><journal-title-group><journal-title xml:lang="en">Ice and Snow</journal-title><trans-title-group xml:lang="ru"><trans-title>Лед и снег</trans-title></trans-title-group></journal-title-group><issn publication-format="print">2076-6734</issn><issn publication-format="electronic">2412-3765</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">688401</article-id><article-id pub-id-type="doi">10.31857/S2076673425020054</article-id><article-id pub-id-type="edn">FPNITV</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Snow cover and avalanches</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Снежный покров и снежные лавины</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">On background observations of the content of trace elements in the solid phase of the snow cover of urban lands</article-title><trans-title-group xml:lang="ru"><trans-title>О фоновых наблюдениях содержания микроэлементов в твёрдой фазе снежного покрова городских земель</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Zakharchenko</surname><given-names>A. V.</given-names></name><name xml:lang="ru"><surname>Захарченко</surname><given-names>А. В.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>avzakh@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Tigeev</surname><given-names>A. A.</given-names></name><name xml:lang="ru"><surname>Тигеев</surname><given-names>А. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>avzakh@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Pas’ko</surname><given-names>O. A.</given-names></name><name xml:lang="ru"><surname>Пасько</surname><given-names>О. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>avzakh@gmail.com</email><xref ref-type="aff" rid="aff2"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Tyumen Scientific Center of the Siberian Branch of the Russian Academy of Sciences (Tyumen Scientific Centre SB RAS)</institution></aff><aff><institution xml:lang="ru">Тюменский научный центр Сибирского отделения Российской академии наук</institution></aff></aff-alternatives><aff-alternatives id="aff2"><aff><institution xml:lang="en">National Open Institute</institution></aff><aff><institution xml:lang="ru">Национальный открытый институт</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2025-09-04" publication-format="electronic"><day>04</day><month>09</month><year>2025</year></pub-date><volume>65</volume><issue>2</issue><issue-title xml:lang="en"/><issue-title xml:lang="ru"/><fpage>255</fpage><lpage>267</lpage><history><date date-type="received" iso-8601-date="2025-07-28"><day>28</day><month>07</month><year>2025</year></date><date date-type="accepted" iso-8601-date="2025-07-28"><day>28</day><month>07</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2025, Zakharchenko A.V., Tigeev A.A., Pas’ko O.A.</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2025, Захарченко А.В., Тигеев А.А., Пасько О.А.</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="en">Zakharchenko A.V., Tigeev A.A., Pas’ko O.A.</copyright-holder><copyright-holder xml:lang="ru">Захарченко А.В., Тигеев А.А., Пасько О.А.</copyright-holder><license><ali:license_ref xmlns:ali="http://www.niso.org/schemas/ali/1.0/">http://creativecommons.org/licenses/by/4.0</ali:license_ref></license></permissions><self-uri xlink:href="https://journals.eco-vector.com/2076-6734/article/view/688401">https://journals.eco-vector.com/2076-6734/article/view/688401</self-uri><abstract xml:lang="en"><p>The problem of background observations is seen in the fact that there are no justifications independent of the researcher for choosing suitable observation points. The high pipes of the emission source allow pollutants to be scattered over long distances, creating a wind shadow near it with a low flow of dust and scattered substances. The points directly adjacent to the source of the emission of pollutants sometimes turn out to have a lower content compared to the remote ones. Therefore, the distance from the source of the emission is not a guarantee of the absence of anthropogenic influence, i.e. natural conditions for the formation of the microelement composition of snow cover dust. As a result, it turns out that the choice of a priori points remote from the urban area in forests and on agricultural land cannot undoubtedly be considered background. Averaging values at such points can lead to the fact that the content of pollutants in them will be higher than at points located in the zone of direct influence of the anthropogenic factor. The choice of background points is made by the authors of studies without an evidence base, which leads to an underestimation or overestimation of the environmental hazard of industrial emissions. Using the example of Tyumen, an algorithm for selecting background observation points, regardless of the observer, is proposed. The territory of the city is divided into squares, and the location of observation points is made randomly. Next, a chain is used: converting the initial data into relative values, hierarchical cluster analysis, calculating the average values of the content of trace elements for all clusters and chemical elements, selecting the cluster with the lowest values, the points of which are taken as the background. The same algorithm can be used for any depositing media: soil, sediments, peat bogs, etc.</p></abstract><trans-abstract xml:lang="ru"><p>Цель работы – решение проблемы отсутствия доказательной базы определения точек исследования как фоновых. Предложена схема, независимая от наблюдателя, позволяющая определить фоновые значения содержания микроэлементов в твёрдой фазе снежного покрова. Применяется следующий ряд: преобразование исходных данных в относительные величины; иерархический кластерный анализ; вычисление средних значений по всем кластерам и химическим элементам; выбор кластера с наименьшими значениями, точки которого принимается за фон.</p></trans-abstract><kwd-group xml:lang="en"><kwd>hierarchical cluster analysis</kwd><kwd>trace elements</kwd><kwd>snow dust</kwd><kwd>classification</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>иерархический кластерный анализ</kwd><kwd>микроэлементы</kwd><kwd>снеговая пыль</kwd><kwd>классификация</kwd></kwd-group><funding-group><funding-statement xml:lang="en">State assignment of the Ministry of Science and Higher Education of the Russian Federation (No. FWRZ-2021-0006).</funding-statement><funding-statement xml:lang="ru">Государственное задание Министерства науки и высшего образования РФ (№ FWRZ-2021-0006).</funding-statement></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><citation-alternatives><mixed-citation xml:lang="en">Bondarevich E.A. 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