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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">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">698993</article-id><article-id pub-id-type="doi">10.7868/S3034648725040047</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>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">OZONE PHOTOCHEMICAL PRODUCTION EFFICIENCY IN NEAR-SURFACE LAYER OVER BOREAL FORESTS OF CENTRAL AND SOUTHERN SIBERIA</article-title><trans-title-group xml:lang="ru"><trans-title>ЭФФЕКТИВНОСТЬ ФОТОХИМИЧЕСКОЙ ГЕНЕРАЦИИ ОЗОНА В ПРИЗЕМНОМ СЛОЕ ВОЗДУХА В БОРЕАЛЬНЫХ ЛЕСАХ ЦЕНТРАЛЬНОЙ И ЮЖНОЙ СИБИРИ</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Moiseenko</surname><given-names>K. B.</given-names></name><name xml:lang="ru"><surname>Моисеенко</surname><given-names>К. Б.</given-names></name></name-alternatives><email>k_moeseyenko@ifaran.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Vasileva</surname><given-names>A. V.</given-names></name><name xml:lang="ru"><surname>Васильева</surname><given-names>А. В.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Belikov</surname><given-names>I. B.</given-names></name><name xml:lang="ru"><surname>Беликов</surname><given-names>И. Б.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Berezina</surname><given-names>E. V.</given-names></name><name xml:lang="ru"><surname>Березина</surname><given-names>Е. В.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Arshinov</surname><given-names>M. Yu.</given-names></name><name xml:lang="ru"><surname>Аршинов</surname><given-names>М. Ю.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff2"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Belan</surname><given-names>B. D.</given-names></name><name xml:lang="ru"><surname>Белан</surname><given-names>Б. Д.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff2"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Obukhov Institute of atmospheric physics RAS</institution></aff><aff><institution xml:lang="ru">Институт физики атмосферы им. А.М. Обухова РАН</institution></aff></aff-alternatives><aff-alternatives id="aff2"><aff><institution xml:lang="en">Zuev Institute of atmospheric optics SB RAS</institution></aff><aff><institution xml:lang="ru">Институт оптики атмосферы им. В.Е. Зуева СО РАН</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2025-08-15" publication-format="electronic"><day>15</day><month>08</month><year>2025</year></pub-date><volume>61</volume><issue>4</issue><issue-title xml:lang="en">VOL 61, NO4 (2025)</issue-title><issue-title xml:lang="ru">ТОМ 61, №4 (2025)</issue-title><fpage>457</fpage><lpage>473</lpage><history><date date-type="received" iso-8601-date="2025-12-21"><day>21</day><month>12</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2025, Russian Academy of Sciences</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2025, Российская академия наук</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="en">Russian Academy of Sciences</copyright-holder><copyright-holder xml:lang="ru">Российская академия наук</copyright-holder><ali:free_to_read xmlns:ali="http://www.niso.org/schemas/ali/1.0/" start_date="2026-08-15"/><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/698993">https://journals.eco-vector.com/0002-3515/article/view/698993</self-uri><abstract xml:lang="en"><p>Quantitative assessments of photochemical ozone production (P<sub>O3</sub>), ozone production efficiency (ΔP) with respect to odd oxygen NO<sub>x</sub> (= NO + NO<sub>2</sub>), and NO<sub>x</sub> exponential lifetime (τ<sub>N</sub>) are estimated from continuous measurements of near-surface mixing ratios of O<sub>3</sub>, NO and NO<sub>2</sub> at the regional stations of ZOTTO (Central Siberia) and Fonovaya (Southern Siberia) in a photochemical active period from March–September. We obtain the general functional forms P<sub>O3</sub> ≈ A·[NO<sub>x</sub>], ΔP = A/(1 + B[NO<sub>x</sub>]), τ<sub>N</sub> = ΔP / A' uniformly valid for the range of the measured NO<sub>x</sub> mixing ratios (0.2–2 ppb), where A' is a proportionality constant in a NO<sub>x</sub>-limiting regime of ozone production, and coefficients A and B depend on the total OH reactivity and exact composition of the CO, CH<sub>4</sub>, and higher hydrocarbons (RH) mixture. We show that atmospheric oxidation of ozone precursors including those emitted from local biogenic sources, along with regional NO<sub>x</sub> emissions, provide an important regional source of O<sub>3</sub> and sink for odd oxygen in the atmospheric boundary layer over boreal forests in the region of study.</p></abstract><trans-abstract xml:lang="ru"><p>По многолетним наблюдениям приземного содержания озона (O<sub>3</sub>) и оксидов азота (NO, NO<sub>2</sub>) на региональных станциях ZOTTO (Zotino Tall Tower Observatory) и «Фоновая» получены оценки скорости фотохимической генерации озона (P<sub>O3</sub>), эффективности наработки озона в расчете на одну молекулу нечетного азота NO<sub>x</sub>(=NO + NO<sub>2</sub>) (ΔP) и времени жизни NO<sub>x</sub> (τ<sub>N</sub>) в фотохимически активные дни с марта по сентябрь. В диапазоне измеренных концентраций NO<sub>x</sub> (0.2–2 млрд<sup>-1</sup>), отвечающих условиям регионально фонового и слабо загрязненного воздуха, имеют место зависимости: P<sub>O3</sub> ≈ A'[NO<sub>x</sub>], ΔP = A/(1 + B[NO<sub>x</sub>]), τ<sub>N</sub> = ΔP/A', где A' — эмпирический коэффициент, A и B — параметры, зависящие от состава воздуха. Для семейства нечетного азота выделены предельные режимы скорости фотохимического стока в условиях высокого и низкого отношения концентрации биогенных углеводородов к концентрации NO<sub>x</sub>. Полученные результаты свидетельствуют о значимом вкладе региональных эмиссий NO<sub>x</sub> и биогенных эмиссий углеводородов в фотохимическую генерацию озона и дневной сток нечетного азота в атмосферном пограничном слое над бореальными лесами Сибири.</p></trans-abstract><kwd-group xml:lang="en"><kwd>ozone</kwd><kwd>NO<sub>x</sub> lifetime</kwd><kwd>biogenic emissions</kwd><kwd>isoprene</kwd><kwd>monoterpenes</kwd><kwd>tropospheric chemistry</kwd><kwd>regional pollution</kwd><kwd>atmospheric boundary layer</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>озон</kwd><kwd>оксиды азота</kwd><kwd>тропосферная фотохимия</kwd><kwd>региональные эмиссии</kwd><kwd>летучие органические соединения</kwd><kwd>предшественники озона</kwd><kwd>атмосферный пограничный слой</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено при поддержке Российского научного фонда в рамках проекта № 20-17-00200 (расчеты и анализ результатов). Подготовка экспериментальных данных по обсерватории ZOTTO выполнены в рамках гос. задания ИФА РАН № 1021042900488-7-1.5.10. Сбор и подготовка экспериментальных данных по обсерватории «Фоновая» выполнены в рамках государственного задания ИФА СО РАН № 121031500342-0.</funding-statement></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Антохин П.Н., Аршинова В.Г., Аршинов М.Ю., Белан Б.Д., Белан С.Б., Давыдов Д.К., Козлов A.B., Краснов O.A., Праслова О.В., Рассказчикова Т.М., Савкин Д.Е., Толмачев Г.Н., Фофонов А.В. Суточная динамика вертикального распределения озона в пограничном слое атмосферы в районе Томска // Оптика атмосф. и океана. 2013. Т. 26. № 8. С. 665–672.</mixed-citation></ref><ref id="B2"><label>2.</label><mixed-citation>Белан Б. Д., Ковалевский В. К., Плотников А. П., Скляднева Т. К. Временная динамика озона и оксидов азота в приземном слое в районе г. Томска // Оптика атмосф. и океана. 1998. Т. 11. № 12. 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