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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">46929</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">Geomagnetic field evolution. Changes on the way?</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Geomagnetic field evolution. Changes on the way?</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Mandea</surname>
       <given-names>Mioara </given-names>
      </name>
      <name xml:lang="en">
       <surname>Mandea</surname>
       <given-names>Mioara </given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Lesur</surname>
       <given-names>Vincent </given-names>
      </name>
      <name xml:lang="en">
       <surname>Lesur</surname>
       <given-names>Vincent </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">Universite Paris Diderot - Institut de Physique du Globe de Paris Geophysique spatiale et planetaire, Paris, France</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Universite Paris Diderot - Institut de Physique du Globe de Paris Geophysique spatiale et planetaire, Paris, France</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Helmholtz-Zentrum Potsdam Deutsches GeoForschungsZentrum - GFZ Sektion, Potsdam, Germany</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Helmholtz-Zentrum Potsdam Deutsches GeoForschungsZentrum - GFZ Sektion, Potsdam, Germany</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>11</volume>
   <issue>3</issue>
   <fpage>1</fpage>
   <lpage>8</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-11-10T01:57:18+03:00">
     <day>10</day>
     <month>11</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46929/view">https://rjes.ru/en/nauka/article/46929/view</self-uri>
   <abstract xml:lang="ru">
    <p>High-quality observations have been obtained from a number of magnetic satellites, complementing the ground available data for the last decade. We present here the issues regarding observatory and satellite data, in order to show how these modern measurements have brought new insights in understanding the Earth's magnetic field. It is only when combined with ground-based data that satellite measurements can provide additional opportunities for studies ranging from core flow, mantle conductivity and lithospheric composition to the dynamics of the ionospheric and magnetospheric currents. Therefore, in this paper a case is presented for the necessity of continuous monitoring of geomagnetic field from ground and space. This contribution is mainly based on some recent work and publications we are co-authoring.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>High-quality observations have been obtained from a number of magnetic satellites, complementing the ground available data for the last decade. We present here the issues regarding observatory and satellite data, in order to show how these modern measurements have brought new insights in understanding the Earth's magnetic field. It is only when combined with ground-based data that satellite measurements can provide additional opportunities for studies ranging from core flow, mantle conductivity and lithospheric composition to the dynamics of the ionospheric and magnetospheric currents. Therefore, in this paper a case is presented for the necessity of continuous monitoring of geomagnetic field from ground and space. This contribution is mainly based on some recent work and publications we are co-authoring.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Geomagnetic field</kwd>
    <kwd>secular variation</kwd>
    <kwd>secular acceleration</kwd>
    <kwd>satellite measurements</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Geomagnetic field</kwd>
    <kwd>secular variation</kwd>
    <kwd>secular acceleration</kwd>
    <kwd>satellite measurements</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
 <back>
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 </back>
</article>
