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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">95199</article-id>
   <article-id pub-id-type="doi">10.2205/2025es001060</article-id>
   <article-id pub-id-type="edn">qvsgki</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">Morphological Features of the Seabed Slope and Their Influence on Cross-Slope Transport of Suspended Matter Under Storm Conditions off the Coast of the Kaliningrad Peninsula</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Морфологические особенности склона дна и их влияние на кросс-склоновый вынос взвешенного вещества в штормовых условиях у берегов Калининградского полуострова</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/0000-0002-3968-9373</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Килесо</surname>
       <given-names>Александр Владимирович</given-names>
      </name>
      <name xml:lang="en">
       <surname>Kileso</surname>
       <given-names>Aleksandr Vladimirovich</given-names>
      </name>
     </name-alternatives>
     <email>aleksandr.kileso@gmail.com</email>
     <bio xml:lang="ru">
      <p>кандидат географических наук;</p>
     </bio>
     <bio xml:lang="en">
      <p>candidate of geographical sciences;</p>
     </bio>
     <xref ref-type="aff" rid="aff-1"/>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
    <contrib contrib-type="author">
     <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-2499-6768</contrib-id>
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Гриценко</surname>
       <given-names>Владимир Алексеевич</given-names>
      </name>
      <name xml:lang="en">
       <surname>Gritsenko</surname>
       <given-names>Vladimir Alekseevich</given-names>
      </name>
     </name-alternatives>
     <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-3"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Балтийский федеральный университет им. Иммануила Канта</institution>
    </aff>
    <aff>
     <institution xml:lang="en">Immanuel Kant Baltic Federal University</institution>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Институт океанологии им. П.П. Ширшова РАН</institution>
     <country>Россия</country>
    </aff>
    <aff>
     <institution xml:lang="en">Shirshov Institute of Oceanology of Russian Academy of Sciences</institution>
     <country>Russian Federation</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-3">
    <aff>
     <institution xml:lang="ru">Институт океанологии им. П.П. Ширшова РАН</institution>
    </aff>
    <aff>
     <institution xml:lang="en">P.P.Shirshov Institute of Oceanology of the Russian Academy of Science</institution>
    </aff>
   </aff-alternatives>
   <pub-date publication-format="print" date-type="pub" iso-8601-date="2025-10-27T00:00:00+03:00">
    <day>27</day>
    <month>10</month>
    <year>2025</year>
   </pub-date>
   <pub-date publication-format="electronic" date-type="pub" iso-8601-date="2025-10-27T00:00:00+03:00">
    <day>27</day>
    <month>10</month>
    <year>2025</year>
   </pub-date>
   <volume>25</volume>
   <issue>5</issue>
   <elocation-id>ES5018</elocation-id>
   <history>
    <date date-type="received" iso-8601-date="2025-02-21T00:00:00+03:00">
     <day>21</day>
     <month>02</month>
     <year>2025</year>
    </date>
    <date date-type="accepted" iso-8601-date="2025-09-08T00:00:00+03:00">
     <day>08</day>
     <month>09</month>
     <year>2025</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/95199/view">https://rjes.ru/en/nauka/article/95199/view</self-uri>
   <abstract xml:lang="ru">
    <p>Приводится описание необходимых условий для возникновения кросс-склонового выноса песка за внешнюю границу прибрежной зоны Калининградского полуострова в юго-восточной части Балтийского моря. Анализ мелкомасштабных градиентных характеристик поверхности подводного берегового склона у отмелых песчаных берегов позволил получить качественные и количественные оценки величин горизонтальных градиентов поверхности склона дна, кривизны и траектории наискорейшего спуска. Были выделены участки подводного берегового склона дна с морфологическими особенностями в виде эрозионных ложбин и каналов с кросссклоновой ориентацией, создающих благоприятные условия для транспорта взвеси в условиях сильных штормов в виде вдольсклоновых суспензионных течений. На основе предложенного в работе критерия выполнена классификация береговой зоны моря у Калининградского полуострова по степени возможного негативного влияния морфологических особенностей склона дна в контексте абразии берега в штормовых условиях.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>An analysis of small-scale gradient characteristics of the underwater coastal slope surface near the shallow sandy shores of the Kaliningrad Peninsula provided qualitative and quantitative estimates of the horizontal gradients of the bottom slope, curvature, and the steepest descent trajectories. Sections of the slope with morphological features such as erosional gullies and cross-slope-oriented channels were identified, creating favorable conditions for suspended sediment transport during severe storms in the form of along-slope suspension currents. Based on the criterion proposed in this study, a classification of the coastal zone near the Kaliningrad Peninsula was carried out according to the degree of negative impact of bottom slope morphological features in the context of potential shoreline erosion under storm conditions.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>подводный береговой склон</kwd>
    <kwd>штормовые условия</kwd>
    <kwd>абразия берегового склона</kwd>
    <kwd>взвесенесущие течения</kwd>
    <kwd>транспорт песка в сторону моря</kwd>
    <kwd>градиентные показатели</kwd>
    <kwd>Калининградский полуостров</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>underwater coastal slope</kwd>
    <kwd>storm conditions</kwd>
    <kwd>coastal slope abrasion</kwd>
    <kwd>suspension currents</kwd>
    <kwd>seaward sand transport</kwd>
    <kwd>gradient parameters</kwd>
    <kwd>Kaliningrad Peninsula</kwd>
   </kwd-group>
   <funding-group>
    <funding-statement xml:lang="ru">Работа выполнена в рамках государственного задания Минобрнауки России для ИО РАН (тема № FMWE-2024-0025).</funding-statement>
    <funding-statement xml:lang="en">The work was carried out within the framework of the state assignment of the Ministry of Education and Science of Russia for the Institute of Oceanology of the Russian Academy of Sciences (topic no. FMWE-2024-0025).</funding-statement>
   </funding-group>
  </article-meta>
 </front>
 <body>
  <p></p>
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