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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Russian Journal of Earth Sciences</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Russian Journal of Earth Sciences</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Russian Journal of Earth Sciences</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">1681-1208</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">88627</article-id>
   <article-id pub-id-type="doi">10.2205/2024ES000951</article-id>
   <article-id pub-id-type="edn">rpkmqq</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>ORIGINAL ARTICLES</subject>
    </subj-group>
    <subj-group>
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">Properties of Short-Period Internal Waves Near Svalbard from Sentinel-1 Satellite Data</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Характеристики короткопериодных внутренних волн в районе архипелага Шпицберген по спутниковым данным Sentinel-1</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-6378-8956</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Козлов</surname>
       <given-names>Игорь Евгеньевич</given-names>
      </name>
      <name xml:lang="en">
       <surname>Kozlov</surname>
       <given-names>Igor E</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-8696-9722</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Михайличенко</surname>
       <given-names>Тамара Витальевна</given-names>
      </name>
      <name xml:lang="en">
       <surname>Mihaylichenko</surname>
       <given-names>Tamara Vital'evna</given-names>
      </name>
     </name-alternatives>
     <email>goldpineapple2020@gmail.com</email>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7246-9885</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Петренко</surname>
       <given-names>Лариса Алексеевна</given-names>
      </name>
      <name xml:lang="en">
       <surname>Petrenko</surname>
       <given-names>Larisa Alekseevna</given-names>
      </name>
     </name-alternatives>
     <email>larcpetr@gmail.com</email>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Морской Гидрофизический Институт РАН</institution>
     <city>Sevastopol’</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Marine Hydrophysical Institute RAS</institution>
     <city>Sevastopol’</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2024-12-12T00:00:00+03:00">
    <day>12</day>
    <month>12</month>
    <year>2024</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2024-12-12T00:00:00+03:00">
    <day>12</day>
    <month>12</month>
    <year>2024</year>
   </pub-date>
   <volume>24</volume>
   <issue>5</issue>
   <fpage>1</fpage>
   <lpage>11</lpage>
   <history>
    <date date-type="received" iso-8601-date="2024-09-13T00:00:00+03:00">
     <day>13</day>
     <month>09</month>
     <year>2024</year>
    </date>
    <date date-type="accepted" iso-8601-date="2024-11-13T00:00:00+03:00">
     <day>13</day>
     <month>11</month>
     <year>2024</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/88627/view">https://rjes.ru/en/nauka/article/88627/view</self-uri>
   <abstract xml:lang="ru">
    <p>В настоящей работе представлены результаты анализа характеристик поля короткопериодных внутренних волн (КВВ) в проливе Фрама и в окрестности архипелага Шпицберген по данным спутниковых измерений Sentinel-1 A/B с июня по сентябрь 2018 г. В ходе обработки 1500 спутниковых радиолокационных изображений (РЛИ) выявлено 750 случаев регистрации поверхностных проявлений КВВ. Максимальное количество проявлений внутренних волн зарегистрировано в августе, когда и условия стратификации, и ледовые условия наиболее благоприятны для генерации и наблюдения КВВ в спутниковых данных. Фоновые метеорологические условия летом 2018 г. привели к отступлению границы дрейфующих льдов на север до 82,5∘ с. ш., что впервые позволило провести детальные наблюдения характеристик внутренних волн над плато Ермак по спутниковым данным. В результате наблюдений выявлены четыре основных района устойчивой генерации КВВ – глубоководная часть пролива Фрама (глубины более 2000 м), юго-западная часть плато Ермак с глубинами 500–1500 м и два района на бровке шельфа в верхней части континентального склона к северо-западу от архипелага Шпицберген с глубинами менее 500 м. Анализ пространственных характеристик КВВ показал, что в районе исследований доминируют пакеты КВВ со средней длиной фронта лидирующей волны около 15 км и средней шириной пакета около 5 км. Самые крупные пакеты КВВ площадью около 400 км2 образуются над плато Ермак, где скорости приливных течений максимальны.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>Here we present the results of observations of short-period internal waves (SIWs) in Fram Strait and near Svalbard based on analysis of Sentinel-1 A/B synthetic aperture radar (SAR) data in June-September 2018. Analysis of 1500 spaceborne SAR images allowed to identify 750 surface signatures of SIWs. Maximal number of SIW identifications is observed in August, when both stratification and ice conditions are favorable for SIW generation and identification in satellite data. Background meteorological conditions in summer 2018 favored the northward movement of the ice boundary up to 82,5 ∘ N that allowed to observe SIWs over the Yermak Plateau. Four main regions of SIW observations were identified – deep Fram Strait region (depths over 2000 m), southwestern Yermak Plateau with depth range of 500–1500 m, and two shelf break/upper continental slope regions northwest from Svalbard with depths below 500 m. Analysis of spatial properties of SIWs has shown that the study region is dominated by SIW trains with a mean crest length of 15 km and mean packet length of about 5 km. The largest SIW trains with area of nearly 400 km2 were observed over the Yermak Plateau where tidal currents are maximal.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>короткопериодные внутренние волны</kwd>
    <kwd>приливные течения</kwd>
    <kwd>турбулентное перемешивание</kwd>
    <kwd>морской лед</kwd>
    <kwd>спутниковая радиолокация морской поверхности</kwd>
    <kwd>пролив Фрама</kwd>
    <kwd>архипелаг Шпицберген</kwd>
    <kwd>плато Ермак</kwd>
    <kwd>Северный Ледовитый океан</kwd>
    <kwd>Арктика</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>short-period internal waves</kwd>
    <kwd>tidal currents</kwd>
    <kwd>turbulent mixing</kwd>
    <kwd>sea ice</kwd>
    <kwd>satellite radar images of the ocean surface</kwd>
    <kwd>Fram Strait</kwd>
    <kwd>Svalbard</kwd>
    <kwd>Yermak Plateau</kwd>
    <kwd>Arctic Ocean</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">Исследование выполнено в рамках государственного задания ФГБУН ФИЦ МГИ по теме № FNNN-2024-0017.</funding-statement>
    <funding-statement xml:lang="en">The study was carried out within the framework of the state assignment of the FSBSI FRC MHI on topic No. FNNN-2024-0017.</funding-statement>
   </funding-group>
  </article-meta>
 </front>
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