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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">hydrophysics</journal-id><journal-title-group><journal-title xml:lang="ru">Фундаментальная и прикладная гидрофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Fundamental and Applied Hydrophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2073-6673</issn><issn pub-type="epub">2782-5221</issn><publisher><publisher-name>St. Petersburg Research Center of the Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-852</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>ФУНДАМЕНТАЛЬНЫЕ ВОПРОСЫ ГИДРОФИЗИКИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>FUNDAMENTAL ISSUES OF HYDROPHYSICS</subject></subj-group></article-categories><title-group><article-title>Транспорт радона и формирование электрического состояния атмосферного пограничного слоя</article-title><trans-title-group xml:lang="en"><trans-title>The radon transport and the atmospheric boundary layer electric state formation</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>Анисимов</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Anisimov</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Ярославская обл., п. Борок</p></bio><bio xml:lang="en"><p>Russian Academy of Sciences, Borok</p></bio><email xlink:type="simple">svga@borok.yar.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>Галиченко</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Galichenko</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Ярославская обл., п. Борок</p></bio><bio xml:lang="en"><p>Russian Academy of Sciences</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Афиногенов</surname><given-names>К. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Aphinogenov</surname><given-names>K. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Ярославская обл., п. Борок</p></bio><bio xml:lang="en"><p>Russian Academy of Sciences, Borok</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Геофизическая обсерватория «Борок» — филиал Института физики Земли им. О. Ю. Шмидта РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Borok Geophysical Observatory of Schmidt Institute of Physics of the Earth</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2016</year></pub-date><pub-date pub-type="epub"><day>18</day><month>11</month><year>2022</year></pub-date><volume>9</volume><issue>4</issue><fpage>7</fpage><lpage>14</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Анисимов С.В., Галиченко С.В., Афиногенов К.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Анисимов С.В., Галиченко С.В., Афиногенов К.В.</copyright-holder><copyright-holder xml:lang="en">Anisimov S.V., Galichenko S.V., Aphinogenov K.V.</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://hydrophysics.spbrc.ru/jour/article/view/852">https://hydrophysics.spbrc.ru/jour/article/view/852</self-uri><abstract><p>Обсуждаются механизмы влияния стратифицированной турбулентности на формирование электрического состояния атмосферного пограничного слоя и вариабельность электрических параметров. В результате натурных наблюдений и численного моделирования установлено, что развитие конвекции в атмосферном пограничном слое приводит к уменьшению электрической проводимости вблизи поверхности земли. Для расчетов использована стохастическая электродинамическая модель, воспроизводящая эволюцию высотных профилей электрической проводимости и напряженности аэроэлектрического поля в невозмущенном осадками и грозовой активностью нижнем слое атмосферы над сушей средних широт. Показано, что связанное с конвекцией усиление генерации турбулентности, сопровождающееся увеличением турбулентной кинетической энергии и дисперсии флуктуаций вертикальной скорости, способствует более интенсивному вертикальному перемешиванию радона и радиоактивных дочерних продуктов. При этом вертикальный перенос радона приводит к более однородному высотному распределению электрической проводимости и увеличению напряженности поля в приземном слое. Выполнены оценки вариабельности электрической проводимости и напряженности аэроэлектрического поля, определяемых эмиссией радона, ионизацией воздуха, разделением зарядов на неоднородностях электрической проводимости, турбулентным транспортом радиоактивных элементов и объемных электрических зарядов. Предполагается, что высотные аэроэлектрические профили могут служить объективными и оперативными параметрами состояния атмосферного пограничного слоя.</p></abstract><trans-abstract xml:lang="en"><p>The mechanisms of influence of stratified turbulence to the formation of the atmospheric boundary layer electric state and the variability of electric parameters are discussed. As a result of the field observations and numerical modeling, it is found that the development of convection in the atmospheric boundary layer reduces the electric conductivity near the surface. The stochastic electrodynamic model, reproducing the evolution of the vertical profiles of electric conductivity and aeroelectric field intensity in the lower troposphere of mid-latitudes land undisturbed by precipitations and thunderstorms, is used for the calculations. The results show that the increased turbulence generation due to convection accompanied by an increase of the turbulent kinetic energy and the variance of vertical turbulent velocity tends to more intensive vertical mixing of radon and its short-lived daughters. In this case, the turbulent transport of radon leads to more uniform vertical distribution of the electric conductivity and an increase of the aeroelectric field intensity in the surface layer. Estimations of the variability of electric conductivity and aeroelectric field intensity, caused by radon emissions, air ionization, charge separation on the electric conductivity inhomogeneities, turbulent transport of radioactive elements and space charge, are performed. It is assumed that altitudinal aeroelectric profiles can be objective and operative parameters of the atmospheric boundary layer turbulent conditions.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>атмосферный пограничный слой</kwd><kwd>турбулентный транспорт</kwd><kwd>вариабельность</kwd><kwd>радон</kwd><kwd>электрическая проводимость</kwd><kwd>электрическое поле</kwd></kwd-group><kwd-group xml:lang="en"><kwd>atmospheric boundary layer</kwd><kwd>turbulent transport</kwd><kwd>variability</kwd><kwd>radon</kwd><kwd>electric conductivity</kwd><kwd>electric field</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено за счет гранта РНФ № 16-17-10209 и частичной финансовой поддержке гранта РФФИ № 15-05-04960.</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">Garratt J. R. The Atmospheric Boundary Layer. 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