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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">sergeogr</journal-id><journal-title-group><journal-title xml:lang="ru">Известия Российской академии наук. Серия географическая</journal-title><trans-title-group xml:lang="en"><trans-title>Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2587-5566</issn><issn pub-type="epub">2658-6975</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.15356/0373-2444-2015-6-48-60</article-id><article-id custom-type="elpub" pub-id-type="custom">sergeogr-325</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>Природные процессы и динамика геосистем</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Natural Processes and Dynamics of Geosystems</subject></subj-group></article-categories><title-group><article-title>НОЧНАЯ И ДНЕВНАЯ ОБЛАЧНОСТЬ ПО РАЗНЫМ СПУТНИКОВЫМ ДАННЫМ</article-title><trans-title-group xml:lang="en"><trans-title>Day and Night Cloudiness Using Satellite Data from Different Sources</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>Чернокульский</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Chernokulsky</surname><given-names>A. V.</given-names></name></name-alternatives><email xlink:type="simple">a.chernokulsky@ifaran.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт физики атмосферы им. А.М. Обухова РАН, Москва, Россия</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, Russia</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2015</year></pub-date><pub-date pub-type="epub"><day>20</day><month>11</month><year>2015</year></pub-date><volume>0</volume><issue>6</issue><fpage>48</fpage><lpage>60</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Чернокульский А.В., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Чернокульский А.В.</copyright-holder><copyright-holder xml:lang="en">Chernokulsky A.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://izvestia.igras.ru/jour/article/view/325">https://izvestia.igras.ru/jour/article/view/325</self-uri><abstract><p>Проведена оценка климатологии дневной и ночной облачности и их разности по различнымспутниковым данным (AIRS-LMD, CERES, MODIS, CALIPSO-GOCCP, PATMOS-x) в сопоставлении с наземными наблюдениями. Выявлено преобладание дневной облачности над сушей и над Северным полушарием в целом, и преобладание ночной облачности над океаном и над Южным полушарием в целом, при этом различия между облачностью над сушей и океаном (и соответственно над Северным и Южным полушариями) сильнее проявляются в ночное время. Региональные значения разности между ночной и дневной облачностью над сушей могут достигать 20–40%, главным образом, в горных районах и в умеренных широтах. Над океаном преобладание ночной облачности отмечено преимущественно в низких широтах (в первую очередь, в восточных частях океанов), где по отдельным данным ночная облачность больше дневной на 15–20%, причём эта разность больше летом. В ряде экваториальных и высокогорных областей Евразии, Африки, Южной Америки и Австралии, а также в северных районах Тихого и Атлантического океанов выявлены существенные различия между данными: согласно одним данным над этими регионами преобладает дневная облачность, согласно другим – ночная. Показано, что время наблюдений может влиять на определение общей облачности. Наблюдения только в дневное время будут завышать значения облачности над сушей (на 20% по сравнению со среднесуточным) и занижать значения облачности над океаном. Наблюдения только в утренние или ночные часы, наоборот, будут занижать значения облачности над сушей (на 8–10%) и завышать над океаном (на 5–7%).</p></abstract><trans-abstract xml:lang="en"><p>Day-time and night-time cloudiness and their difference were assessed based on various satellite data (AIRS-LMD, CERES, MODIS, CALIPSO-GOCCP, PATMOS-x) and surface observations. It was found that day-time cloudiness prevails over land and over the entire Northern Hemisphere while night-time cloudiness prevails over the ocean and over the Southern Hemisphere, moreover difference between cloudiness over land and over the ocean (and consequently over both hemispheres) is higher at the nighttime.Regionally, difference between day-time and night-time cloudiness over land is up to 20–40%, mostly over mountain regions and midlatitudes. Over the ocean, night-time cloudiness prevails in low latitudes in summer (mostly over the eastern parts of the oceans) where it is up to 15–20% more than day-time cloudiness. A disagreement between different data is noted over the vast equatorial and highmountain regions in Eurasia, Africa, South America, Australia, North Pacifi c and North Atlantic. Particularly,some data display that day-time cloudiness prevails in that regions, other data shows the opposite. It was shown, that time of observations can affect the estimate of total cloudiness. Though, only day-time measurements lead to an overestimation of cloudiness over land (up to 20% of the total daily cloudiness) and underestimation over the ocean. On the contrary, only night-time observations (or observations at the morning) lead to an overestimation of cloudiness over the ocean (up to 5–7%) and underestimation over land (up to 8–10%). Regional differences are even more suffi cient.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>дневная и ночная облачность</kwd><kwd>суточный ход облачности</kwd><kwd>общая облачность</kwd><kwd>спутниковые данные</kwd><kwd>региональные различия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>day-time and night-time cloudiness</kwd><kwd>diurnal cycle of cloudiness</kwd><kwd>total clouduness</kwd><kwd>satellite data</kwd><kwd>regional differences</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">Кобзарь А.И. Прикладная математическая статистика. Для инженеров и научных работников. М.: Физматлит, 2006. 816 с.</mixed-citation><mixed-citation xml:lang="en">Кобзарь А.И. Прикладная математическая статистика. Для инженеров и научных работников. 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