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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="ru"><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">698997</article-id><article-id pub-id-type="doi">10.7868/S3034648725040086</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">RELATION OF CO<sub>2</sub> CONCENTRATION TO METEOROLOGICAL CONDITIONS AND ATMOSPHERIC WAVE PROCESSES NEAR EAST ANTARCTICA</article-title><trans-title-group xml:lang="ru"><trans-title>СВЯЗЬ КОНЦЕНТРАЦИИ СО<sub>2</sub> ВБЛИЗИ ВОСТОЧНОЙ АНТАРКТИДЫ С МЕТЕОРОЛОГИЧЕСКИМИ УСЛОВИЯМИ И АТМОСФЕРНЫМИ ВОЛНОВЫМИ ПРОЦЕССАМИ</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Marchuk</surname><given-names>E. A.</given-names></name><name xml:lang="ru"><surname>Марчук</surname><given-names>Е. А.</given-names></name></name-alternatives><email>murchuk-ekaterin@mail.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Chunchuzov</surname><given-names>I. P.</given-names></name><name xml:lang="ru"><surname>Чунчузов</surname><given-names>И. П.</given-names></name></name-alternatives><email>igor.chunchuzov@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Repina</surname><given-names>I. A.</given-names></name><name xml:lang="ru"><surname>Репина</surname><given-names>И. А.</given-names></name></name-alternatives><email>murchuk-ekaterin@mail.ru</email><xref ref-type="aff" rid="aff1"/><xref ref-type="aff" rid="aff2"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Ivanov</surname><given-names>B. V.</given-names></name><name xml:lang="ru"><surname>Иванов</surname><given-names>Б. В.</given-names></name></name-alternatives><email>murchuk-ekaterin@mail.ru</email><xref ref-type="aff" rid="aff3"/><xref ref-type="aff" rid="aff4"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Bezgreshnov</surname><given-names>A. M.</given-names></name><name xml:lang="ru"><surname>Безгрешнов</surname><given-names>А. М.</given-names></name></name-alternatives><email>murchuk-ekaterin@mail.ru</email><xref ref-type="aff" rid="aff3"/></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">Lomonosov Moscow State University, Research Computing Center</institution></aff><aff><institution xml:lang="ru">Московский государственный университет им. М.В. Ломоносова, Научно-исследовательский вычислительный центр</institution></aff></aff-alternatives><aff-alternatives id="aff3"><aff><institution xml:lang="en">Arctic and Antarctic Research Institute</institution></aff><aff><institution xml:lang="ru">Арктический и антарктический научно-исследовательский институт</institution></aff></aff-alternatives><aff-alternatives id="aff4"><aff><institution xml:lang="en">Saint-Petersburg State University</institution></aff><aff><institution xml:lang="ru">Санкт-Петербургский государственный университет</institution></aff></aff-alternatives><content-language>ru</content-language><pub-date date-type="pub" publication-format="electronic" iso-8601-date="2025-08-15"><day>15</day><month>08</month><year>2025</year></pub-date><pub-date date-type="collection"><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>519</fpage><lpage>537</lpage><history><date date-type="received" iso-8601-date="2025-12-21"><day>21</day><month>12</month><year>2025</year></date></history><pub-history><event event-type="received"><event-desc>Received:<date date-type="received" iso-8601-date="2025-12-21"><day>21</day><month>12</month><year>2025</year></date></event-desc></event><event event-type="pub"><event-desc>Published:<pub-date date-type="pub" publication-format="electronic" iso-8601-date="2025-08-15"><day>15</day><month>08</month><year>2025</year></pub-date></event-desc></event></pub-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/698997">https://journals.eco-vector.com/0002-3515/article/view/698997</self-uri><abstract xml:lang="en"><p>The present study analyses the dependence of CO<sub>2</sub> concentration on meteorological parameters and wave processes in the atmosphere. This analysis was based on data obtained during the 68-th Russian Antarctic Expedition on the Scientific expedition ship “Akademik Fedorov” (December 2022 — February 2023). Common spectral maxima in cross-spectra of temporal variations of meteorological parameters (atmospheric pressure, temperature and wind speed) and CO<sub>2</sub> concentration in a wide range of periods (from ten minutes to a day) were analyzed. The oscillations with a discrete set of periods from ten minutes to a day were detected in the frequency spectra and cross-spectra of fluctuations of meteorological parameters and turbulent fluxes of momentum and heat, A possible mechanism of formation of the observed frequency spectra of variations of meteorological parameters and CO<sub>2</sub> concentration is proposed. It is connected with the influence of the nonlinear process of advection of internal waves in the varying wind caused by solar tides (diurnal and semidiurnal) and the total field of internal waves from their regular sources (solar terminator) and irregular sources (meteorological fronts, orography, jet currents, convection and etc).</p></abstract><trans-abstract xml:lang="ru"><p>Проведен анализ зависимости концентрации СО<sub>2</sub> от метеорологических параметров и волновых процессов в атмосфере на основе данных, полученных в рамках 68-й Российской антарктической экспедиции на НЭС «Академик Федоров» (декабрь 2022 г. – февраль 2023 г.). Проанализированы общие спектральные максимумы в кросс-спектрах временных вариаций метеопараметров (атмосферного давления, температуры и скорости ветра) и концентрации СО<sub>2</sub> в широком диапазоне периодов: от десяти минут до суток. В частотных спектрах и кросс-спектрах флуктуаций метеопараметров и турбулентных потоков импульса и тепла обнаружены колебания с дискретным набором периодов от десяти минут до суток. Предложен возможный механизм формирования наблюдаемых частотных спектров вариаций метеопараметров и концентрации СО<sub>2</sub>. Он связан с влиянием нелинейного процесса адвекции внутренних волн в переменном поле скорости ветра, создаваемого солнечными приливами (суточным и полусуточным) и суммарным полем внутренних волн от их регулярных источников (солнечный терминатор) и нерегулярных источников (метеофронты, орография, струйные течения, конвекция и др.).</p></trans-abstract><kwd-group xml:lang="en"><kwd>atmospheric internal gravity waves</kwd><kwd>solar terminator</kwd><kwd>wave-induced advection</kwd><kwd>spectral analysis</kwd><kwd>East Antarctica</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>атмосферные внутренние гравитационные волны</kwd><kwd>солнечный терминатор</kwd><kwd>индуцируемая волнами адвекция</kwd><kwd>спектральный анализ</kwd><kwd>Восточная Антарктида</kwd></kwd-group><funding-group/></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Гармаш С.В., Линьков Е.М., Петрова Л.Н., Швед Г.М. 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