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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">46559</article-id>
   <article-id pub-id-type="doi">10.2205/2020ES000738</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">Cloudiness over the oceans at subarctic latitudes as a visible part of atmospheric moisture transport</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Cloudiness over the oceans at subarctic latitudes as a visible part of atmospheric moisture transport</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Aleksandrova</surname>
       <given-names>M </given-names>
      </name>
      <name xml:lang="en">
       <surname>Aleksandrova</surname>
       <given-names>M </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Shirshov Institute of Oceanology RAS</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Shirshov Institute of Oceanology RAS</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>21</volume>
   <issue>1</issue>
   <history>
    <date date-type="received" iso-8601-date="2021-10-29T12:48:48+03:00">
     <day>29</day>
     <month>10</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46559/view">https://rjes.ru/en/nauka/article/46559/view</self-uri>
   <abstract xml:lang="ru">
    <p>The article analyzes the climatology and interannual variability of fractional total and low cloud cover in the subarctic and subpolar regions of the North Atlantic and the North Pacific. We used surface visual observations of cloudiness from voluntary observing ships (VOS) for the period from 1950 to 2017. It is shown that in the North Atlantic and the North Pacific seasonal variations of the mean cloud cover demonstrate contrasting character. For a better identification of regional features, the probability distributions of the fractional cloud cover were analyzed. Analysis of interannual variability shows that in many areas of the North Atlantic and the North Pacific, significant linear trends in both total and low cloud cover are observed. Moreover, in the North Pacific, linear trends in the total cloudiness have pronounced seasonality.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>The article analyzes the climatology and interannual variability of fractional total and low cloud cover in the subarctic and subpolar regions of the North Atlantic and the North Pacific. We used surface visual observations of cloudiness from voluntary observing ships (VOS) for the period from 1950 to 2017. It is shown that in the North Atlantic and the North Pacific seasonal variations of the mean cloud cover demonstrate contrasting character. For a better identification of regional features, the probability distributions of the fractional cloud cover were analyzed. Analysis of interannual variability shows that in many areas of the North Atlantic and the North Pacific, significant linear trends in both total and low cloud cover are observed. Moreover, in the North Pacific, linear trends in the total cloudiness have pronounced seasonality.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Subarctic cloudiness</kwd>
    <kwd>visual cloud observation</kwd>
    <kwd>cloud climatology over the ocean</kwd>
    <kwd>long-term trends in cloud cover</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Subarctic cloudiness</kwd>
    <kwd>visual cloud observation</kwd>
    <kwd>cloud climatology over the ocean</kwd>
    <kwd>long-term trends in cloud cover</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="en">This work was funded by the Russian Ministry of Science and Higher Education (agreement \\# 05.616.21.0112, project ID RFMEFI61619X0112).</funding-statement>
   </funding-group>
  </article-meta>
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