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  <front>
    <journal-meta>
      <journal-id journal-id-type="publisher-id">Physical Oceanography</journal-id>
      <journal-title-group>
        <journal-title xml:lang="en">Physical Oceanography</journal-title>
      </journal-title-group>
      <issn publication-format="print">1573-160X</issn>
    </journal-meta>
    <article-meta>
      <article-id pub-id-type="publisher-id">20240201</article-id>

      <article-categories>
        <subj-group subj-group-type="toc-heading" xml:lang="en">
          <subject>Thermohydrodynamics of the ocean and the atmosphere</subject>
        </subj-group>
        <subj-group subj-group-type="article-type">
          <subject>Research Article</subject>
        </subj-group>
      </article-categories>

      <title-group>
        <article-title xml:lang="en">Finite-Difference Approximation of the Potential Vorticity Equation for a Stratified Incompressible Fluid and an Example of its Application for Modeling the Black Sea Circulation</article-title>
        <subtitle>Part I. Finite-Difference Equation of Potential Vorticity of Ideal Fluid</subtitle>
      </title-group>

      <contrib-group>
        <contrib contrib-type="author">
          <contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-5405-2282</contrib-id>
          <contrib-id contrib-id-type="researcherid">C-1729-2016</contrib-id>
          <name>
            <surname>Demyshev</surname>
            <given-names>S. G.</given-names>
          </name>
          <address>
            <country country="RU">Russian Federation</country>
          </address>
          <email>demyshev@gmail.com</email>
          <xref ref-type="aff" rid="aff1"/>
        </contrib>
      </contrib-group>

      <aff id="aff1">
        <institution>Marine Hydrophysical Institute of RAS</institution>
        <addr-line>Sevastopol</addr-line>
        <country country="RU">Russia</country>
      </aff>

      <pub-date date-type="pub" iso-8601-date="2024-04-30" publication-format="electronic">
        <day>30</day>
        <month>04</month>
        <year>2024</year>
      </pub-date>
      <volume>31</volume>
      <issue>2</issue>
      <fpage>149</fpage>
      <lpage>160</lpage>

      <history>
        <date date-type="received" iso-8601-date="2023-06-09">
          <day>09</day>
          <month>06</month>
          <year>2023</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="2023-07-25">
          <day>25</day>
          <month>07</month>
          <year>2023</year>
        </date>
        <date date-type="accepted" iso-8601-date="2023-01-18">
          <day>18</day>
          <month>01</month>
          <year>2023</year>
        </date>
      </history>

      <permissions>
        <copyright-statement xml:lang="en">Copyright ©; 2024, S. G. Demyshev</copyright-statement>
        <copyright-year>2024</copyright-year>
        <copyright-holder xml:lang="en">S. G. Demyshev</copyright-holder>
        <ali:free_to_read xmlns:ali="http://www.niso.org/schemas/ali/1.0/"/>
        <license>
          <ali:license_ref xmlns:ali="http://www.niso.org/schemas/ali/1.0/">https://creativecommons.org/licenses/by-nc/4.0/</ali:license_ref>
        </license>
      </permissions>

      <self-uri xlink:href="https://physical-oceanography.ru/repository/issues/2024/02/01/" xlink:title="Article page">https://physical-oceanography.ru/repository/issues/2024/02/01/</self-uri>

      <abstract xml:lang="en">
        <p><bold>Purpose.</bold> The study is purposed at deriving the discrete equations of absolute and potential vorticity for a three-dimensional stratified incompressible fluid as an exact consequence of the finite-difference equations of sea dynamics in the field of a potential mass force in the adiabatic approximation provided that viscosity and diffusion are absent. The properties of two-dimensional projections of the absolute vorticity equation onto coordinate planes and the three-dimensional potential vorticity equation are analyzed.</p>
        <p><bold>Methods and results.</bold> In order to determine the discrete analogues of absolute and potential vorticity, an additional grid is introduced, where the finite-difference equations for the components both of absolute and potential vorticity are written down. Two-dimensional analogues of the three-dimensional equation of absolute vorticity on the planes (<italic>x</italic>, <italic>y</italic>), (<italic>y</italic>, <italic>z</italic>) and (<italic>x</italic>, <italic>z</italic>) are obtained; they possess the feature of preserving vorticity, energy and enstrophy (square of vorticity). A discrete equation for potential vorticity of a stratified incompressible fluid is derived from the finite-difference system of three-dimensional equations of sea dynamics in the adiabatic approximation at the absence of viscosity and diffusion.</p>
        <p><bold>Conclusions.</bold> In the case of a linear equation of state, the discrete equations of absolute vorticity and potential vorticity which are the exact consequence of finite-difference formulation are obtained. The equation of potential vorticity is of a divergent form, and two-dimensional analogues of the absolute vorticity equation on the planes (<italic>x</italic>, <italic>y</italic>), (<italic>y</italic>, <italic>z</italic>) and (<italic>x</italic>, <italic>z</italic>) have two quadratic invariants that provide preservation of the average wave number.</p>
      </abstract>

      <kwd-group>
        <kwd>discrete equation</kwd>
        <kwd>dynamics of sea</kwd>
        <kwd>kinetic energy</kwd>
        <kwd>vortex</kwd>
        <kwd>potential vorticity</kwd>
        <kwd>Ertel invariant</kwd>
      </kwd-group>

      <funding-group>
        <funding-statement xml:lang="en">The study was carried out with financial support of the Russian Science Foundation grant 23-27-00141.</funding-statement>
      </funding-group>
    </article-meta>
  </front>

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