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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">6a9c15dd32807fdbab86e867</article-id>
   <article-id pub-id-type="doi">10.2205/2026es001107</article-id>
   <article-id pub-id-type="edn">dastnl</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">Statistics of Wave Heights, Crests, and Troughs During the Black Sea Storm in November 2023</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Statistics of Wave Heights, Crests, and Troughs During the Black Sea Storm in November 2023</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-4412-2483</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Гармашов</surname>
       <given-names>Антон Викторович</given-names>
      </name>
      <name xml:lang="en">
       <surname>Garmashov</surname>
       <given-names>Anton Viktorovich</given-names>
      </name>
     </name-alternatives>
     <email>garmashov@mhi-ras.ru</email>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-9942-2796</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Запевалов</surname>
       <given-names>Александр Сергеевич</given-names>
      </name>
      <name xml:lang="en">
       <surname>Zapevalov</surname>
       <given-names>Aleksander Sergeevich</given-names>
      </name>
     </name-alternatives>
     <email>sevzepter@mail.ru</email>
     <bio xml:lang="ru">
      <p>доктор физико-математических наук;доктор физико-математических наук;</p>
     </bio>
     <bio xml:lang="en">
      <p>doctor of physical and mathematical sciences;doctor of physical and mathematical sciences;</p>
     </bio>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Морской  гидрофизический  институт  РАН</institution>
     <country country="RU" xml:lang="ru">Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Marine Hydrophysical Institute of the Russian Academy of Sciences</institution>
     <country country="RU" xml:lang="en">Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Морской гидрофизический институт РАН</institution>
     <city xml:lang="ru">Севастополь</city>
     <country country="RU" xml:lang="ru">Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Marine Hydrophysical Institute, Russian Academy of Sciences</institution>
     <city xml:lang="en">Sevastopol</city>
     <country country="RU" xml:lang="en">Russian Federation</country>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2026-09-18T11:59:13+03:00">
    <day>18</day>
    <month>09</month>
    <year>2026</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2026-09-18T11:59:13+03:00">
    <day>18</day>
    <month>09</month>
    <year>2026</year>
   </pub-date>
   <volume>26</volume>
   <issue>3</issue>
   <elocation-id>ES3019</elocation-id>
   <history>
    <date date-type="received" iso-8601-date="2025-07-02T00:00:00+03:00">
     <day>02</day>
     <month>07</month>
     <year>2025</year>
    </date>
    <date date-type="accepted" iso-8601-date="2026-03-02T00:00:00+03:00">
     <day>02</day>
     <month>03</month>
     <year>2026</year>
    </date>
   </history>
   <permissions>
    <copyright-statement xml:lang="ru">© 2026 Гармашов А.В., Запевалов А.С.</copyright-statement>
    <copyright-statement xml:lang="en">© 2026 Garmashov A.V., Zapevalov A.S.</copyright-statement>
    <copyright-year>2026</copyright-year>
    <copyright-holder xml:lang="ru">Гармашов Антон Викторович, Запевалов Александр Сергеевич</copyright-holder>
    <copyright-holder xml:lang="en">Garmashov Anton Viktorovich, Zapevalov Aleksander Sergeevich</copyright-holder>
   </permissions>
   <self-uri xlink:href="https://rjes.ru/en/nauka/publications/6a9c15dd32807fdbab86e867/view">https://rjes.ru/en/nauka/publications/6a9c15dd32807fdbab86e867/view</self-uri>
   <abstract xml:lang="ru">
    <p>The changes in the characteristics of freak waves during an extreme storm in the Black Sea in November 2023 were analyzed based on direct measurement data from a stationary oceanographic platform located off the southern coast of Crimea. The height of individual waves reached up to 7.2 m, with a maximum significant height of 3.7 m. The continuous three-day wave record was divided into 20-min fragments, for which statistical characteristics of the waves were calculated. Three types of abnormality indices were analyzed based on the excess of wave height, crest height, and trough depth over a given level. During the storm, all abnormality indices increased, indicating that the probability of freak wave occurrences was higher than under ordinary conditions. When the significant wave height exceeded 2 m, it was often observed that the trough depth was greater than the crest height.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>The changes in the characteristics of freak waves during an extreme storm in the Black Sea in November 2023 were analyzed based on direct measurement data from a stationary oceanographic platform located off the southern coast of Crimea. The height of individual waves reached up to 7.2 m, with a maximum significant height of 3.7 m. The continuous three-day wave record was divided into 20-min fragments, for which statistical characteristics of the waves were calculated. Three types of abnormality indices were analyzed based on the excess of wave height, crest height, and trough depth over a given level. During the storm, all abnormality indices increased, indicating that the probability of freak wave occurrences was higher than under ordinary conditions. When the significant wave height exceeded 2 m, it was often observed that the trough depth was greater than the crest height.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>extreme storm</kwd>
    <kwd>freak waves</kwd>
    <kwd>crest</kwd>
    <kwd>trough</kwd>
    <kwd>abnormality index</kwd>
    <kwd>excess kurtosis</kwd>
    <kwd>Black Sea</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>extreme storm</kwd>
    <kwd>freak waves</kwd>
    <kwd>crest</kwd>
    <kwd>trough</kwd>
    <kwd>abnormality index</kwd>
    <kwd>excess kurtosis</kwd>
    <kwd>Black Sea</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">This work was completed within the framework of the state assignment on the topic FNNN-2024-0014 “Fundamental studies of interaction processes in the sea-air system that form the physical state variability of the marine environment at various spatial and temporal scales”.</funding-statement>
    <funding-statement xml:lang="en">This work was completed within the framework of the state assignment on the topic FNNN-2024-0014 “Fundamental studies of interaction processes in the sea-air system that form the physical state variability of the marine environment at various spatial and temporal scales”.</funding-statement>
   </funding-group>
  </article-meta>
 </front>
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