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  <journal-meta>
   <journal-id journal-id-type="publisher-id">Solar-Terrestrial Physics</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Solar-Terrestrial Physics</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Solar-Terrestrial Physics</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">2500-0535</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">49624</article-id>
   <article-id pub-id-type="doi">10.12737/stp-82202209</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>Results of current research</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>Results of current research</subject>
    </subj-group>
    <subj-group>
     <subject>Results of current research</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">Comparative analysis of variability in the mid-latitude stratosphere and ionosphere in winter periods</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Comparative analysis of variability in the mid-latitude stratosphere and ionosphere in winter periods</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Ясюкевич</surname>
       <given-names>Анна Сергеевна</given-names>
      </name>
      <name xml:lang="en">
       <surname>Yasyukevich</surname>
       <given-names>Anna Sergeevna</given-names>
      </name>
     </name-alternatives>
     <email>annpol@iszf.irk.ru</email>
     <bio xml:lang="ru">
      <p>кандидат физико-математических наук;</p>
     </bio>
     <bio xml:lang="en">
      <p>candidate of physical and mathematical sciences;</p>
     </bio>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Веснин</surname>
       <given-names>Артем Михайлович</given-names>
      </name>
      <name xml:lang="en">
       <surname>Vesnin</surname>
       <given-names>Artem Mihaylovich</given-names>
      </name>
     </name-alternatives>
     <email>artem_vesnin@iszf.irk.ru</email>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Институт солнечно-земной физики СО РАН</institution>
     <city>Иркутск</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of Solar Terrestrial Physics SB RAS</institution>
     <city>Irkutsk</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Институт солнечно-земной физики СО РАН</institution>
     <city>Иркутск</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of Solar Terrestrial Physics SB RAS</institution>
     <city>Irkutsk</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2022-06-30T12:52:48+03:00">
    <day>30</day>
    <month>06</month>
    <year>2022</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2022-06-30T12:52:48+03:00">
    <day>30</day>
    <month>06</month>
    <year>2022</year>
   </pub-date>
   <volume>8</volume>
   <issue>2</issue>
   <fpage>61</fpage>
   <lpage>68</lpage>
   <history>
    <date date-type="received" iso-8601-date="2022-04-02T00:00:00+03:00">
     <day>02</day>
     <month>04</month>
     <year>2022</year>
    </date>
    <date date-type="accepted" iso-8601-date="2022-04-21T00:00:00+03:00">
     <day>21</day>
     <month>04</month>
     <year>2022</year>
    </date>
   </history>
   <self-uri xlink:href="https://zh-szf.ru/en/nauka/article/49624/view">https://zh-szf.ru/en/nauka/article/49624/view</self-uri>
   <abstract xml:lang="ru">
    <p>In this work, we perform a joint analysis of the spatial-temporal dynamics of ionospheric and stratospheric variability (with scales characteristic of internal gravity waves) at different longitudes of midlatitudes of the Northern Hemisphere. We analyze the winter periods of 2012–2013 and 2018–2019 when strong midwinter sudden stratospheric warmings (SSWs) occurred. An increase in the variability in the stratosphere is shown to occur in a limited latitude interval 40°–60° N in the region of existence of a winter circumpolar vortex. Under SSW conditions, the generation of wave disturbances in the stratosphere ceases manifesting itself in a significant decrease in the stratospheric variability index. Similar behavior is noted in the spatial-temporal dynamics of the index of the total electron content variability. The level of ionospheric variability at midlatitudes decreases significantly after SSW peaks. The decrease in the ionospheric variability can be explained by a reduction in wave generation in the stratosphere, associated with the destruction of the circumpolar vortex during SSWs</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>In this work, we perform a joint analysis of the spatial-temporal dynamics of ionospheric and stratospheric variability (with scales characteristic of internal gravity waves) at different longitudes of midlatitudes of the Northern Hemisphere. We analyze the winter periods of 2012–2013 and 2018–2019 when strong midwinter sudden stratospheric warmings (SSWs) occurred. An increase in the variability in the stratosphere is shown to occur in a limited latitude interval 40°–60° N in the region of existence of a winter circumpolar vortex. Under SSW conditions, the generation of wave disturbances in the stratosphere ceases manifesting itself in a significant decrease in the stratospheric variability index. Similar behavior is noted in the spatial-temporal dynamics of the index of the total electron content variability. The level of ionospheric variability at midlatitudes decreases significantly after SSW peaks. The decrease in the ionospheric variability can be explained by a reduction in wave generation in the stratosphere, associated with the destruction of the circumpolar vortex during SSWs</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>ionosphere</kwd>
    <kwd>total electron content</kwd>
    <kwd>variability</kwd>
    <kwd>internal gravity waves</kwd>
    <kwd>stratosphere</kwd>
    <kwd>circumpolar vortex</kwd>
    <kwd>sudden stratospheric warmings</kwd>
    <kwd>atmosphere-ionosphere interaction</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>ionosphere</kwd>
    <kwd>total electron content</kwd>
    <kwd>variability</kwd>
    <kwd>internal gravity waves</kwd>
    <kwd>stratosphere</kwd>
    <kwd>circumpolar vortex</kwd>
    <kwd>sudden stratospheric warmings</kwd>
    <kwd>atmosphere-ionosphere interaction</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">The work was financially supported by RSF (Grant No. 20-77-00070)</funding-statement>
    <funding-statement xml:lang="en">The work was financially supported by RSF (Grant No. 20-77-00070)</funding-statement>
   </funding-group>
  </article-meta>
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