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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">izmertech</journal-id><journal-title-group><journal-title xml:lang="ru">Измерительная техника</journal-title><trans-title-group xml:lang="en"><trans-title>Izmeritel`naya Tekhnika</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0368-1025</issn><issn pub-type="epub">2949-5237</issn><publisher><publisher-name>ФГУП "ВНИИФТРИ"</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">izmertech-429</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>ОПТИКО-ФИЗИЧЕСКИЕ ИЗМЕРЕНИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>OPTICOPHYSICAL MEASUREMENTS</subject></subj-group></article-categories><title-group><article-title>Использование статистически неоднородных экранов в задаче калибровки лидара по параметрам изображений частиц для приземного слоя атмосферы</article-title><trans-title-group xml:lang="en"><trans-title></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>Арумов</surname><given-names>Г. П.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.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>Бухарин</surname><given-names>А. В.</given-names></name></name-alternatives><email xlink:type="simple">tumbul@iki.rssi.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>Тюрин</surname><given-names>А. В.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Институт космических исследований РАН</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2014</year></pub-date><pub-date pub-type="epub"><day>07</day><month>02</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>36</fpage><lpage>40</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Арумов Г.П., Бухарин А.В., Тюрин А.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Арумов Г.П., Бухарин А.В., Тюрин А.В.</copyright-holder><copyright-holder xml:lang="en">Арумов Г.П., Бухарин А.В., Тюрин А.В.</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://www.izmt.ru/jour/article/view/429">https://www.izmt.ru/jour/article/view/429</self-uri><abstract><p>Найдено эквивалентное сечение полидисперсных и несферических частиц с использованием статистически неоднородных экранов. Предложен метод обеспечения дистанционных измерений концентрации частиц в приземном слое атмосферы.</p></abstract><trans-abstract xml:lang="en"><p>The equivalent section of polydisperse and non-spherical particles with use of statistically inhomogeneous screens has been found. The proposed method can be used for metrological assurance of particle concentration in the atmosphere surface layer.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>дистанционное зондирование</kwd><kwd>двухпозиционная схема</kwd><kwd>функция распределения частиц</kwd><kwd>рассеивающий объект</kwd><kwd>несферические</kwd><kwd>поли- и монодисперсные частицы</kwd><kwd>лидар</kwd><kwd>remote sensing</kwd><kwd>two-position scheme</kwd><kwd>particle distribution function</kwd><kwd>scattering object</kwd><kwd>non-spherical</kwd><kwd>poly- and monodisperse particles</kwd><kwd>lidar</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Мак Картни Э. Оптика атмосферы. / пер. с англ. М.: МИР, 1979.</mixed-citation><mixed-citation xml:lang="en">Мак Картни Э. Оптика атмосферы. / пер. с англ. 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