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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">aari</journal-id><journal-title-group><journal-title xml:lang="ru">Проблемы Арктики и Антарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Antarctic Research</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0555-2648</issn><issn pub-type="epub">2618-6713</issn><publisher><publisher-name>Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.30758/0555-2648-2022-68-2-96-117</article-id><article-id custom-type="elpub" pub-id-type="custom">aari-440</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>ОКЕАНОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>OCEANOLOGY</subject></subj-group></article-categories><title-group><article-title>Применение данных судового телевизионного комплекса в оперативном гидрометеорологическом обеспечении морской деятельности на примере картирования толщины ледяного покрова в Арктике</article-title><trans-title-group xml:lang="en"><trans-title>Mapping the thickness of sea ice in the Arctic as an example of using data from a ship-based television complex for operational hydrometeorological support of maritime activities</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>Афанасьева</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Afanasyeva</surname><given-names>E. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург,</p><p>Москва</p></bio><bio xml:lang="en"><p>Ekaterina V. Afanasyeva</p><p>St. Petersburg,</p><p>Moscow</p></bio><email xlink:type="simple">afanasieva@aari.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>Сероветников</surname><given-names>С. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Serovetnikov</surname><given-names>S. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Sergei S. Serovetnikov</p><p>St. Petersburg</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Алексеева</surname><given-names>Т. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Alekseeva</surname><given-names>T. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург,</p><p>Москва</p></bio><bio xml:lang="en"><p>Tatiana A. Alekseeva</p><p>St. Petersburg,</p><p>Moscow</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>Гришин</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Grishin</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Evgeniy A. Grishin</p><p>St. Petersburg</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Солодовник</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Solodovnik</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Aleksandr A. Solodovnik</p><p>St. Petersburg</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Филиппов</surname><given-names>Н. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Filippov</surname><given-names>N. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург</p></bio><bio xml:lang="en"><p>Nikita A. Filippov</p><p>St. Petersburg</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ГНЦ РФ Арктический и антарктический научно-исследовательский институт;&#13;
Институт космических исследований РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute;&#13;
Space Research Institute of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>ГНЦ РФ Арктический и антарктический научно-исследовательский институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>State Scientific Center of the Russian Federation Arctic and Antarctic Research Institute</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>03</day><month>07</month><year>2022</year></pub-date><volume>68</volume><issue>2</issue><fpage>96</fpage><lpage>117</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Афанасьева Е.В., Сероветников С.С., Алексеева Т.А., Гришин Е.А., Солодовник А.А., Филиппов Н.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Афанасьева Е.В., Сероветников С.С., Алексеева Т.А., Гришин Е.А., Солодовник А.А., Филиппов Н.А.</copyright-holder><copyright-holder xml:lang="en">Afanasyeva E.V., Serovetnikov S.S., Alekseeva T.A., Grishin E.A., Solodovnik A.A., Filippov N.A.</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.aaresearch.science/jour/article/view/440">https://www.aaresearch.science/jour/article/view/440</self-uri><abstract><p>В работе поднят вопрос о необходимости получения достоверных натурных данных о толщине ледяного покрова для обеспечения более высокой точности информационной продукции, выпускаемой национальными ледовыми службами, в частности ледовых карт, которые являются базовым элементом оперативного гидрометеорологического обеспечения морской деятельности в пределах Северного морского пути (СМП) и примыкающих к нему акваториях. Предложено решение проблемы путем размещения на современных атомных ледоколах и судах усиленного ледового класса Arc7 автоматизированных судовых телевизионных метеорологических комплексов (СТМК), позволяющих получать достоверные данные о толщине льда и других сопутствующих гидрометеорологических параметрах непосредственно во время движения судна во льдах. В настоящее время растущее число судов усиленного ледового класса является единственной доступной по экономическим причинам инфраструктурой, пригодной для развертывания наземной распределенной сети оперативного мониторинга гидрометеорологических условий на трассах СМП.</p></abstract><trans-abstract xml:lang="en"><p>Sea ice charts produced by the ice services of the world are among the most widely used sources of information about sea ice conditions in the Arctic. The absolute majority of sea ice charts are based on visual expert analysis of satellite imagery accompanied by auxiliary data including ground information from coastal stations and ships navigating the Northern Sea Route (NSR). Ground measurements of sea ice thickness are necessary for validating the results of satellite imagery interpretation. Shipboard observations are highly valuable because, unlike coastal stations, the ships provide information about sea ice cover straight on the navigational routes, not in the coastal areas of land-fast ice, where the thickness values are not fully representative of the ice in the open sea. However, the current system of shipboard observations used by commercial fleets often does not meet the reliability requirements due to the human factor involved in the process of data collection. In the early 2000s, the Arctic and Antarctic Research Institute (AARI) suggested a new methodology for shipboard ice thickness measurement. A ship-based television complex (STC) was developed in order to exclude the human factor and standardize observations. The inaccuracy value was estimated as 3.8 % of the real thickness. By 2018, STC had been upgraded to a new ship-based television meteorological complex (STMC) allowing continuous automatic measurement of ice thickness and many other related hydrometeorological parameters during the entire voyage. The automatic and autonomous operation of the new equipment allows placing it on board the ship without the need for an ice specialist to be permanently present. It means that STMC can be used by commercial fleets, which constantly increase the number of Arc7 ice class vessels they use. For economic reasons, reinforced ice class vessels, whose number is growing, represent the only available infrastructure suitable for the deployment of distributed network providing operational hydrometeorological monitoring on the NSR. A comparison of STC data with AARI ice charts has revealed that real-time transmission of STC data from ships to the ice service office could increase the accuracy of ice charts and, as a consequence, the quality of the entire system of hydrometeorological informational support of maritime activities in the Arctic.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Арктика</kwd><kwd>дистанционное зондирование</kwd><kwd>ледовая карта</kwd><kwd>ледовая навигация</kwd><kwd>натурные измерения</kwd><kwd>Северный морской путь</kwd><kwd>судовой телевизионный комплекс</kwd><kwd>толщина льда</kwd></kwd-group><kwd-group xml:lang="en"><kwd>the Arctic</kwd><kwd>ground measurements</kwd><kwd>ice thickness</kwd><kwd>Northern Sea Route</kwd><kwd>remote sensing</kwd><kwd>sea ice chart</kwd><kwd>sea ice navigation</kwd><kwd>ship-based television complex</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках НИТР НИУ Росгидромета на 2021– 2024 гг. по теме 5.1.2. Развитие существующих и разработка новых методов и технологий долгосрочного (месячного и сезонного) прогнозирования элементов ледово-гидрологического режима арктических морей, низовьев и устьевых областей рек в условиях климатических изменений. Анализ спутниковых данных выполнялся в рамках темы «Мониторинг» гос. регистрация № 122042500031-8</funding-statement><funding-statement xml:lang="en">The analysis of satellite data was carried out within the framework of the topic “Monitoring”, state registration no. 122042500031-8</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">Афанасьева Е.В., Алексеева Т.А., Соколова Ю.В., Демчев Д.М., Чуфарова М.С., БыченковЮ.Д., Девятаев О.С. Методика составления ледовых карт ААНИИ // Российская Арктика. 2019. № 7. 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