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    Hi everyone,<br>
    <br>
    <p>Thanks a lot for your comments and help. Following your
      recommendations, I’m attaching two figures and the namelists. </p>
    <p>Fig1.jpg shows the MEDSEA parent model, with my domain marked by
      a red rectangle, as well as the three points where I plotted the
      SSH from the parent model.</p>
    Fig2.jpg contains three subplots. The top panel corresponds to the
    SouthWest of Sicily, where I compare the SSH at that point with and
    without tides from the MEDSEA model. I also include the MEDSEA SSH
    averaged over my domain (black line) shared in all plots and the
    MITgcm output (my result) shown as a black dashed line. I repeat
    this comparison in the south of my domain (cyan) and in Gibraltar
    (red).<br>
    <br>
    Note: The Y-axis scales are not shared between subplots, but in all
    cases, it's clear that the parent model shows a low frequency SSH
    signal that I’m currently unable to reproduce in MITgcm.<br>
    As you mentioned, probably I should disable the balanced flow
    option. Additionally, I’m sharing the namelists data and data.obcs,
    if you have any advice or suggestions, I’d be happy to try them.<br>
    <br>
    Thanks again for your help!<br>
    Best regards,<br>
    <p>Jordi</p>
    <p><br>
    </p>
    <div class="moz-cite-prefix">On 8/7/25 17:24, Martin Losch wrote:<br>
    </div>
    <blockquote type="cite"
      cite="mid:45C12C69-2106-44E7-9A07-44252775F1BC@awi.de">
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      Hi Jordi,
      <div><br>
      </div>
      <div>it would help if you could provide your namelist files. And
        maybe the customised *_OPTIONS.h files, if they are very
        different from the standard ones.</div>
      <div>Do you use open boundary conditions? Balanced flow is maybe
        an issue?</div>
      <div><br>
      </div>
      <div>Martin</div>
      <div>
        <div><br>
          <blockquote type="cite">
            <div>On 8. Jul 2025, at 16:57, Dimitris Menemenlis
              <a class="moz-txt-link-rfc2396E" href="mailto:dmenemenlis@gmail.com"><dmenemenlis@gmail.com></a> wrote:</div>
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              <div
style="overflow-wrap: break-word; -webkit-nbsp-mode: space; line-break: after-white-space;">Hi
                Jodi, perhaps a good place to start would be to
                understand cause of the larger oscillations in MEDSEA
                and ROMS, which might then help you diagnose what is
                missing in your MITgcm configuration.  For example, if
                the ~10-day oscillation in MEDSEA and ROMS is primarily
                caused by transport through Gibraltar Strait, then you
                could look at MITgcm’s transport through Gibraltar
                Strait to see whether it has been correctly prescribed.
                <div><br>
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                <div>D.<br id="lineBreakAtBeginningOfMessage">
                  <div><br>
                    <blockquote type="cite">
                      <div>On Jul 8, 2025, at 6:13 AM, Jordi Iglesias
                        <a class="moz-txt-link-rfc2396E" href="mailto:jiglesias@icm.csic.es"><jiglesias@icm.csic.es></a> wrote:</div>
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                          <p>Dear MITgcm community,<br>
                            <br>
                            Over the past few months, I’ve been
                            struggling to achieve realistic sea surface
                            height ("Eta") results in my MITgcm
                            simulations. I’ve tried several
                            configurations,including non-hydrostatic,
                            quasi-non-hydrostatic, and nonlinear free
                            surface options, but the SSH output often
                            differs significantly from the parent model
                            (the Copernicus Mediterranean analysis,
                            MEDSEA). I’ve attached an example and also
                            shared a link to illustrate the issue. I
                            have tides configured, and the ssh is
                            initialized from MEDSEA data. However, when
                            I compare the SSH output with the parent
                            model (or with a ROMS simulation, for
                            example), it appears to oscillate around a
                            constant value that doesn’t evolve much over
                            time, or changes are very small.<br>
                            <br>
                            A summary of my configuration: Horizontal
                            resolution: 1.6 km, NW Mediterranean Sea,
                            Atmospheric forcing: ECMWF, initial ssh set
                            with pSurfInitFile, SphericalPolarGrid,
                            quasiHydrostatic = .TRUE., nonlinFreeSurf =
                            3, rigidLid = .FALSE., implicitFreeSurface =
                            .TRUE., <br>
                          </p>
                          <p>If any additional parameters would help
                            diagnose the issue, I’d be happy to provide
                            them.<br>
                            <br>
                            The temperature, salinity, and velocity
                            fields are generally in good agreement with
                            ROMS and MEDSEA, but I’d really like to
                            improve the SSH performance. Has anyone
                            encountered a similar issue or found
                            strategies to improve SSH in MITgcm?<br>
                            <br>
                            Thanks in advance for your help!<br>
                            <br>
                            Best regards,<br>
                            Jordi<br>
                            <br>
                            <a class="moz-txt-link-freetext"
href="https://saco.csic.es/s/c2fSgN5RWPRcDSQ" moz-do-not-send="true">https://saco.csic.es/s/c2fSgN5RWPRcDSQ</a><br>
                          </p>
                          <p><br>
                          </p>
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