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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">48386</article-id>
   <article-id pub-id-type="doi">10.2205/2021ES000777</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">Features of suspended matter distribution at the atmosphere-water boundary in the Atlantic and Southern Oceans</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Features of suspended matter distribution at the atmosphere-water boundary in the Atlantic and Southern Oceans</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Nemirovskaya</surname>
       <given-names>I. A.</given-names>
      </name>
      <name xml:lang="en">
       <surname>Nemirovskaya</surname>
       <given-names>I. A.</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Gordeev</surname>
       <given-names>V. V.</given-names>
      </name>
      <name xml:lang="en">
       <surname>Gordeev</surname>
       <given-names>V. V.</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">Shirshov Institute of Oceanology RAS</institution>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Shirshov Institute of Oceanology RAS</institution>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Shirshov Institute of Oceanology RAS</institution>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Shirshov Institute of Oceanology RAS</institution>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2022-01-26T00:00:00+03:00">
    <day>26</day>
    <month>01</month>
    <year>2022</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2022-01-26T00:00:00+03:00">
    <day>26</day>
    <month>01</month>
    <year>2022</year>
   </pub-date>
   <volume>21</volume>
   <issue>5</issue>
   <fpage>1</fpage>
   <lpage>16</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-05-20T00:00:00+03:00">
     <day>20</day>
     <month>05</month>
     <year>2021</year>
    </date>
    <date date-type="accepted" iso-8601-date="2021-09-21T00:00:00+03:00">
     <day>21</day>
     <month>09</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="http://rjes.wdcb.ru/v21/2021ES000777/2021ES000777.pdf">http://rjes.wdcb.ru/v21/2021ES000777/2021ES000777.pdf</self-uri>
   <abstract xml:lang="ru">
    <p>The new results of studying the particle size distribution of aerosol, suspended matter and organic compounds in the suspended matter of surface waters of the South and Atlantic Oceans along the Africa-Antarctic-Southern America-English Channel route are presented. The measurements show that the fraction of 0-3 µm prevails in the particle size distribution of aerosols. The maximum amount of aerosols was found in the coastal regions of Europe (on average 29,353 p/L), and the minimum - in the coastal regions of Antarctica (on average 5197 p/L), that is due to the Antarctic ice cover on the continent. In surface waters, the distribution of suspended particulate matter and organic matter in it is mainly influenced by the frontal zones. In the Antarctic region, the development of phytoplankton at the ice - water interface in the surface water layer leads to an increase in the concentrations of suspended particulate matter and chlorophyll a and, to a lesser extent, of lipids and hydrocarbons. In the open waters of the arid oceanic zones, the influx of aerosols from the atmosphere has the most significant effect on the formation of suspended matter and organic matter in surface waters in comparison with the another parts of the oceans.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>The new results of studying the particle size distribution of aerosol, suspended matter and organic compounds in the suspended matter of surface waters of the South and Atlantic Oceans along the Africa-Antarctic-Southern America-English Channel route are presented. The measurements show that the fraction of 0-3 µm prevails in the particle size distribution of aerosols. The maximum amount of aerosols was found in the coastal regions of Europe (on average 29,353 p/L), and the minimum - in the coastal regions of Antarctica (on average 5197 p/L), that is due to the Antarctic ice cover on the continent. In surface waters, the distribution of suspended particulate matter and organic matter in it is mainly influenced by the frontal zones. In the Antarctic region, the development of phytoplankton at the ice - water interface in the surface water layer leads to an increase in the concentrations of suspended particulate matter and chlorophyll a and, to a lesser extent, of lipids and hydrocarbons. In the open waters of the arid oceanic zones, the influx of aerosols from the atmosphere has the most significant effect on the formation of suspended matter and organic matter in surface waters in comparison with the another parts of the oceans.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Aerosols</kwd>
    <kwd>surface water</kwd>
    <kwd>suspended particulate matter</kwd>
    <kwd>organic matter</kwd>
    <kwd>𝐶org</kwd>
    <kwd>chlorophyll a; lipids</kwd>
    <kwd>hydrocarbons</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Aerosols</kwd>
    <kwd>surface water</kwd>
    <kwd>suspended particulate matter</kwd>
    <kwd>organic matter</kwd>
    <kwd>𝐶org</kwd>
    <kwd>chlorophyll a; lipids</kwd>
    <kwd>hydrocarbons</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">The authors are grateful to A. M. Titova and H. V. Kozina for their assistance in sampling, A. G. Boev and A. V. Khramtsova for as- sistance in conducting the analyses. The authors are grateful to the comments of the anonymous reviewers whose effort and suggestions have helped to make this a stronger contribution.</funding-statement>
    <funding-statement xml:lang="en">The authors are grateful to A. M. Titova and H. V. Kozina for their assistance in sampling, A. G. Boev and A. V. Khramtsova for as- sistance in conducting the analyses. The authors are grateful to the comments of the anonymous reviewers whose effort and suggestions have helped to make this a stronger contribution.</funding-statement>
   </funding-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
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