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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">46607</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">Intra-annual variations of intensity of subsurface currents and surface water temperature in the southwestern part of the Barents Sea inferred from drifter data</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Intra-annual variations of intensity of subsurface currents and surface water temperature in the southwestern part of the Barents Sea inferred from drifter data</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Nikitin</surname>
       <given-names>O P</given-names>
      </name>
      <name xml:lang="en">
       <surname>Nikitin</surname>
       <given-names>O P</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Zhukovskaya</surname>
       <given-names>A O</given-names>
      </name>
      <name xml:lang="en">
       <surname>Zhukovskaya</surname>
       <given-names>A O</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">N. N. Zubov State Oceanographic Institute</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">N. N. Zubov State Oceanographic Institute</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">N. N. Zubov State Oceanographic Institute</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">N. N. Zubov State Oceanographic Institute</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>16</volume>
   <issue>3</issue>
   <fpage>1</fpage>
   <lpage>7</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-10-29T12:53:32+03:00">
     <day>29</day>
     <month>10</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46607/view">https://rjes.ru/en/nauka/article/46607/view</self-uri>
   <abstract xml:lang="ru">
    <p>The paper presents a description of observations of near-surface currents and water temperature at the surface, made in the Barents Sea and in the south-western part of the Kara Sea with the help of satellite tracked drifting buoys -- drifters. This information should be taken into account when planning further drifter observations in the considered area. For the southwestern region of the Barents Sea -- the most covered by drifter observations~--~the intra-annual variations of the averaged velocity module of currents at the depth of 15~m and the average temperature at the water surface are calculated. It is shown that the currents intensify in winter and weaken in summer with a minimum of the velocity module in August. Water temperature at the surface, on the contrary, has a maximum in August, and a minimum is reached in April.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>The paper presents a description of observations of near-surface currents and water temperature at the surface, made in the Barents Sea and in the south-western part of the Kara Sea with the help of satellite tracked drifting buoys -- drifters. This information should be taken into account when planning further drifter observations in the considered area. For the southwestern region of the Barents Sea -- the most covered by drifter observations~--~the intra-annual variations of the averaged velocity module of currents at the depth of 15~m and the average temperature at the water surface are calculated. It is shown that the currents intensify in winter and weaken in summer with a minimum of the velocity module in August. Water temperature at the surface, on the contrary, has a maximum in August, and a minimum is reached in April.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>drifter observations</kwd>
    <kwd>subsurface currents</kwd>
    <kwd>surface water temperature</kwd>
    <kwd>annual course</kwd>
    <kwd>Barents Sea</kwd>
    <kwd>Kara Sea</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>drifter observations</kwd>
    <kwd>subsurface currents</kwd>
    <kwd>surface water temperature</kwd>
    <kwd>annual course</kwd>
    <kwd>Barents Sea</kwd>
    <kwd>Kara Sea</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
 <back>
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</article>
