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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">46884</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">Possible connection of electric field variations with the size of ice particles in the polar stratosphere</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Possible connection of electric field variations with the size of ice particles in the polar stratosphere</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Belikov</surname>
       <given-names>Yu E</given-names>
      </name>
      <name xml:lang="en">
       <surname>Belikov</surname>
       <given-names>Yu E</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Nikolaishvili</surname>
       <given-names>S Sh</given-names>
      </name>
      <name xml:lang="en">
       <surname>Nikolaishvili</surname>
       <given-names>S Sh</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">Institute of Applied Geophysics, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of Applied Geophysics, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Institute of Applied Geophysics, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of Applied Geophysics, Moscow, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>12</volume>
   <issue>4</issue>
   <fpage>1</fpage>
   <lpage>2</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-11-10T00:55:12+03:00">
     <day>10</day>
     <month>11</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46884/view">https://rjes.ru/en/nauka/article/46884/view</self-uri>
   <abstract xml:lang="ru">
    <p>The hypothesis is proposed that ice particles of polar stratospheric clouds PSCs are charged and trapped by the Earth's electric field. This hypothesis explains the absence or the lowest vertical transport of chlorine species and allows the assumption of the essential dependence of the sizes of ice particles on the magnitude of the Earth's electric field in the stratosphere. This assumption means that the ozone content in the stratosphere is closely connected to variations in the magnitude of the electric field. This conclusion is justified by experimental observations.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>The hypothesis is proposed that ice particles of polar stratospheric clouds PSCs are charged and trapped by the Earth's electric field. This hypothesis explains the absence or the lowest vertical transport of chlorine species and allows the assumption of the essential dependence of the sizes of ice particles on the magnitude of the Earth's electric field in the stratosphere. This assumption means that the ozone content in the stratosphere is closely connected to variations in the magnitude of the electric field. This conclusion is justified by experimental observations.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Ozone</kwd>
    <kwd>polar stratospheric clouds</kwd>
    <kwd>Earth's electric field</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Ozone</kwd>
    <kwd>polar stratospheric clouds</kwd>
    <kwd>Earth's electric field</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
 <back>
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  </ref-list>
 </back>
</article>
