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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="other" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Izvestiya, Atmospheric and Oceanic Physics</journal-id><journal-title-group><journal-title xml:lang="en">Izvestiya, Atmospheric and Oceanic Physics</journal-title><trans-title-group xml:lang="ru"><trans-title>Известия РАН. Физика атмосферы и океана</trans-title></trans-title-group></journal-title-group><issn publication-format="print">0002-3515</issn><issn publication-format="electronic">3034-6487</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">658281</article-id><article-id pub-id-type="doi">10.31857/S0002351523050024</article-id><article-id pub-id-type="edn">CWHTFZ</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Articles</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Статьи</subject></subj-group><subj-group subj-group-type="article-type"><subject></subject></subj-group></article-categories><title-group><article-title xml:lang="en">Electricity of the Undisturbed Atmospheric Boundary Layer of Middle Latitudes</article-title><trans-title-group xml:lang="ru"><trans-title>Электричество невозмущенного атмосферного пограничного слоя средних широт</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Anisimov</surname><given-names>S. V.</given-names></name><name xml:lang="ru"><surname>Анисимов</surname><given-names>С. В.</given-names></name></name-alternatives><email>svga@borok.yar.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Aphinogenov</surname><given-names>K. V.</given-names></name><name xml:lang="ru"><surname>Афиногенов</surname><given-names>К. В.</given-names></name></name-alternatives><email>svga@borok.yar.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Galichenko</surname><given-names>S. V.</given-names></name><name xml:lang="ru"><surname>Галиченко</surname><given-names>С. В.</given-names></name></name-alternatives><email>svga@borok.yar.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Prokhorchuk</surname><given-names>A. A.</given-names></name><name xml:lang="ru"><surname>Прохорчук</surname><given-names>А. А.</given-names></name></name-alternatives><email>svga@borok.yar.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Klimanova</surname><given-names>E. V.</given-names></name><name xml:lang="ru"><surname>Климанова</surname><given-names>Е. В.</given-names></name></name-alternatives><email>svga@borok.yar.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Kozmina</surname><given-names>A. S.</given-names></name><name xml:lang="ru"><surname>Козьмина</surname><given-names>А. С.</given-names></name></name-alternatives><email>svga@borok.yar.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Guriev</surname><given-names>A. V.</given-names></name><name xml:lang="ru"><surname>Гурьев</surname><given-names>А. В.</given-names></name></name-alternatives><email>svga@borok.yar.ru</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Borok Geophysical Observatory, Schmidt Institute of Physics of the Earth, Russian Academy of Sciences</institution></aff><aff><institution xml:lang="ru">Геофизическая обсерватория “Борок” – филиал Федерального государственного бюджетного учреждения науки Института физики Земли им. О.Ю. Шмидта Российской академии наук (ГО “Борок” ИФЗ РАН)</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2023-09-01" publication-format="electronic"><day>01</day><month>09</month><year>2023</year></pub-date><volume>59</volume><issue>5</issue><fpage>595</fpage><lpage>611</lpage><history><date date-type="received" iso-8601-date="2025-02-20"><day>20</day><month>02</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2023, С.В. Анисимов, К.В. Афиногенов, С.В. Галиченко, А.А. Прохорчук, Е.В. Климанова, А.С. Козьмина, А.В. Гурьев</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2023, С.В. Анисимов, К.В. Афиногенов, С.В. Галиченко, А.А. Прохорчук, Е.В. Климанова, А.С. Козьмина, А.В. Гурьев</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="en">С.В. Анисимов, К.В. Афиногенов, С.В. Галиченко, А.А. Прохорчук, Е.В. Климанова, А.С. Козьмина, А.В. Гурьев</copyright-holder><copyright-holder xml:lang="ru">С.В. Анисимов, К.В. Афиногенов, С.В. Галиченко, А.А. Прохорчук, Е.В. Климанова, А.С. Козьмина, А.В. Гурьев</copyright-holder><license><ali:license_ref xmlns:ali="http://www.niso.org/schemas/ali/1.0/">https://creativecommons.org/licenses/by-nc-nd/4.0</ali:license_ref></license></permissions><self-uri xlink:href="https://journals.eco-vector.com/0002-3515/article/view/658281">https://journals.eco-vector.com/0002-3515/article/view/658281</self-uri><abstract xml:lang="en"><p id="idm45181323662576">The atmospheric boundary layer is the lowermost part of the atmosphere, the turbulent dynamics and electrodynamics of which are determined by the complex organization of processes in a dissipative environment with energy input from many sources. Regions of the atmosphere undisturbed by thunderstorms and precipitation are characterized by low-energy electrical processes, for the study of which requires a developed instrument base and knowledge of the methods of synchronous spaced high-precision measurements of several physical quantities. The paper presents the results of recent studies of electricity of the atmospheric boundary layer of mid-latitudes carried out using the measuring complex of Borok Geophysical Observatory IPE RAS and numerical modeling. Quantitative estimates of the average values and variability of small ion concentration, the corresponding components of electrical conductivity, and atmospheric electric field intensity are performed. Two types of electric structures formed by the electric current flow through a turbulent medium with inhomogeneous conductivity are defined.</p></abstract><trans-abstract xml:lang="ru"><p id="idm45181323660832">Атмосферный пограничный слой представляет собой нижнюю часть атмосферы, турбулентная динамика и электродинамика которой определяются сложной организацией процессов в диссипативной среде с поступлением энергии от многих источников. Невозмущенные грозовой активностью и осадками области атмосферы характеризуются электрическими процессами с низкой энергией, для исследования которых требуется наличие развитой приборной базы и владение методами синхронных разнесенных высокоточных измерений нескольких физических величин. В работе приводятся результаты недавних исследований электричества невозмущенного атмосферного пограничного слоя средних широт, проводимых с помощью измерительного комплекса Геофизической обсерватории “Борок” ИФЗ РАН и численного моделирования. Выполнены количественные оценки средних значений и вариабельности концентраций легких атмосферных ионов, соответствующих полярных компонент электрической проводимости воздуха и напряженности атмосферного электрического поля. Определены два типа электрических структур, формируемых при протекании тока в турбулентной среде с неоднородной электрической проводимостью.</p></trans-abstract><kwd-group xml:lang="en"><kwd>atmospheric boundary layer</kwd><kwd>geophysical observations</kwd><kwd>atmospheric electricity</kwd><kwd>atmospheric small ions</kwd><kwd>radon</kwd><kwd>statistical self-similarity</kwd><kwd>electrical structures</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>атмосферный пограничный слой</kwd><kwd>геофизические наблюдения</kwd><kwd>атмосферное электричество</kwd><kwd>атмосферные легкие ионы</kwd><kwd>радон</kwd><kwd>статистическое самоподобие</kwd><kwd>электрические структуры</kwd></kwd-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Анисимов С.В., Галиченко С.В., Афиногенов К.В., Макрушин А.П., Шихова Н.М. Объемная активность радона и ионообразование в невозмущенной нижней атмосфере: наземные наблюдения и численное моделирование // Изв. 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