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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Solnechno-Zemnaya Fizika</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Solnechno-Zemnaya Fizika</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Солнечно-земная физика</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">2712-9640</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">97195</article-id>
   <article-id pub-id-type="doi">10.12737/szf-114202507</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>Результаты  исследований</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>Results of current research</subject>
    </subj-group>
    <subj-group>
     <subject>Результаты  исследований</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">Numerical modeling of spatial perturbations of the ionosphere from local tropospheric sources</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Численное моделирование пространственных возмущений ионосферы от локальных тропосферных источников</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Карпов</surname>
       <given-names>Иван Викторович</given-names>
      </name>
      <name xml:lang="en">
       <surname>Karpov</surname>
       <given-names>Ivan Viktorovich</given-names>
      </name>
     </name-alternatives>
     <email>ivkarpov@inbox.ru</email>
     <bio xml:lang="ru">
      <p>доктор физико-математических наук;</p>
     </bio>
     <bio xml:lang="en">
      <p>doctor of physical and mathematical sciences;</p>
     </bio>
     <xref ref-type="aff" rid="aff-1"/>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Бессараб</surname>
       <given-names>Федор Семенович</given-names>
      </name>
      <name xml:lang="en">
       <surname>Bessarab</surname>
       <given-names>Fedor Semenovich</given-names>
      </name>
     </name-alternatives>
     <email>FBESSARAB@kantiana.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-3"/>
     <xref ref-type="aff" rid="aff-4"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Борчевкина</surname>
       <given-names>Ольга Павловна</given-names>
      </name>
      <name xml:lang="en">
       <surname>Borchevkina</surname>
       <given-names>Olga Pavlovna</given-names>
      </name>
     </name-alternatives>
     <email>opsuslova@gmail.com</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-5"/>
     <xref ref-type="aff" rid="aff-6"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Калининградский филиал Института земного магнетизма, ионосферы и распространения радиоволн им. Н.В. Пушкова РАН</institution>
     <city>Калининград</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">West Department of Pushkov Institute of Terrestrial Mag-netism, Ionosphere and Radio Wave Propagation RAS</institution>
     <city>Kaliningrad</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Балтийский федеральный университет имени И. Канта</institution>
     <city>Калининград</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">I. Kant Baltic Federal University</institution>
     <city>Kaliningrad</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-3">
    <aff>
     <institution xml:lang="ru">Калининградский филиал Института земного магнетизма, ионосферы и распространения радиоволн им. Н.В. Пушкова РАН</institution>
     <city>Калининград</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">West Department of Pushkov Institute of Terrestrial Mag-netism, Ionosphere and Radio Wave Propagation RAS</institution>
     <city>Kaliningrad</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-4">
    <aff>
     <institution xml:lang="ru">Балтийский федеральный университет имени И. Канта</institution>
     <city>Калининград</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">I. Kant Baltic Federal University</institution>
     <city>Kaliningrad</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-5">
    <aff>
     <institution xml:lang="ru">Калининградский филиал Института земного магнетизма, ионосферы и распространения радиоволн им. Н.В. Пушкова РАН</institution>
     <city>Калининград</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">West Department of Pushkov Institute of Terrestrial Mag-netism, Ionosphere and Radio Wave Propagation RAS</institution>
     <city>Kaliningrad</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-6">
    <aff>
     <institution xml:lang="ru">Балтийский федеральный университет имени И. Канта</institution>
     <city>Калининград</city>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">I. Kant Baltic Federal University</institution>
     <city>Kaliningrad</city>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2025-12-10T11:21:27+03:00">
    <day>10</day>
    <month>12</month>
    <year>2025</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2025-12-10T11:21:27+03:00">
    <day>10</day>
    <month>12</month>
    <year>2025</year>
   </pub-date>
   <volume>11</volume>
   <issue>4</issue>
   <fpage>71</fpage>
   <lpage>78</lpage>
   <history>
    <date date-type="received" iso-8601-date="2025-04-07T00:00:00+03:00">
     <day>07</day>
     <month>04</month>
     <year>2025</year>
    </date>
    <date date-type="accepted" iso-8601-date="2025-05-10T00:00:00+03:00">
     <day>10</day>
     <month>05</month>
     <year>2025</year>
    </date>
   </history>
   <self-uri xlink:href="https://zh-szf.ru/en/nauka/article/97195/view">https://zh-szf.ru/en/nauka/article/97195/view</self-uri>
   <abstract xml:lang="ru">
    <p>В работе представлены результаты моделирования пространственно-временных возмущений термосферы во время сильного метеорологического возмущения. Моделирование выполнено с использованием Глобальной самосогласованной модели термосферы, ионосферы и протоносферы (ГСМ ТИП). Воздействие тропосферных/стратосферных источников на термосферу при диссипации акустических и внутренних гравитационных волн, генерируемых в области метеорологического шторма, учитывалось в ГСМ ТИП путем задания дополнительного теплового источника на высоте 120 км. Результаты моделирования эффектов циклона в октябре 2017 г. показали, что действие локального дополнительного источника нагрева термосферы приводит к возмущениям параметров термосферы и ионосферы как непосредственно над областью источника, так и на значительном удалении от него. В области дополнительного нагрева отмечается понижение полного электронного содержания (ТЕС), достигающее в дневное время 20 % по сравнению с метеорологически-спокойным днем. Южнее и восточнее области локализации источника отмечаются положительные возмущения ТЕС с относительными амплитудами 5–10 % в дневное время. Физические процессы, определяющие реакцию ионосферы непосредственно в области источника, обусловлены нагревом термосферы и его влиянием на изменения нейтрального состава и циркуляции нейтрального ветра. Возмущения ТЕС в областях, удаленных от области источника, определяются динамическими процессами, которые приводят к переносу плазмы в восточном направлении и смещению ионосферных возмущений к низким широтам.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>The paper presents the results of modeling of spatial and temporal perturbations of the thermosphere during a strong meteorological disturbance. The modeling was performed using the Global Self-Consistent Model of the thermosphere, ionosphere, and protonosphere (GSM TIP). The impact of tropospheric/stratospheric sources on the thermosphere during dissipation of acoustic and internal gravity waves, generated in the meteorological storm region, was considered in GSM TIP by specifying an additional thermal source. The results of modeling of ionospheric effects of the meteorological storm in October 2017 have shown that the action of a local additional source of heating of the thermosphere leads to perturbations of the thermosphere and ionosphere parameters both directly above the source region and at a significant distance from it. In additional heating of the thermosphere, a decrease is observed in the total electron content (TEC) values, reaching 20 % in the daytime compared to a meteorologically quiet day. To the south and east of the source region, there are positive TEC perturbations with relative amplitudes 5–10 % during the daytime. The physical processes determining the ionospheric response directly in the source region are conditioned by heating of the thermosphere and its influence on changes in the neutral composition and circulation of the neutral wind. The TEC perturbations in the regions remote from the source region are determined by dynamic processes, which lead to the eastward transport of plasma and displacement of ionospheric perturbations to low latitudes.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>полное электронное содержание</kwd>
    <kwd>термосфера</kwd>
    <kwd>ионосфера</kwd>
    <kwd>акустические волны</kwd>
    <kwd>внутренние гравитационные волны</kwd>
    <kwd>численное моделирование</kwd>
    <kwd>метеорологический шторм</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>total electron content</kwd>
    <kwd>thermosphere</kwd>
    <kwd>ionosphere</kwd>
    <kwd>acoustic waves</kwd>
    <kwd>internal gravity waves</kwd>
    <kwd>numerical modeling</kwd>
    <kwd>meteorological storm</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">Исследование выполнено за счет гранта Российского научного фонда № 25-27-00213 [https://rscf.ru/project/25-27-00213/]</funding-statement>
    <funding-statement xml:lang="en">The research was financially supported by the Russian Science Foundation (Grant No. 25-27-00213) [https://rscf.ru/project/25-27-00213/]</funding-statement>
   </funding-group>
  </article-meta>
 </front>
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