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      <dc:title>Evidence of reflected internal solitary waves in the Strait of Gibraltar.</dc:title>
      <dc:creator>Roustan, Jean-Baptiste</dc:creator>
      <dc:creator>Bordois, Lucie</dc:creator>
      <dc:creator>García-Lafuente, Jesús</dc:creator>
      <dc:creator>Dumas, Frank</dc:creator>
      <dc:creator>Auclair, Francis</dc:creator>
      <dc:creator>Carton, Xavier</dc:creator>
      <dc:subject>Oceanografía fisica</dc:subject>
      <dc:subject>Oleaje</dc:subject>
      <dc:subject>Hidrodinámica</dc:subject>
      <dc:subject>Gibraltar (Estrecho)</dc:subject>
      <dc:description>Large‐amplitude internal solitary waves (ISWs) propagating eastward toward the Alboran Sea&#xd;
have long been known in the Strait of Gibraltar. New in‐situ data and satellite images evidence northwestward&#xd;
propagating ISWs. These waves are probably the reflection of the well‐known eastward propagating wave along&#xd;
the Moroccan shelf. A simple 2D‐vertical section, run with the compressible non‐hydrostatic Coastal and&#xd;
Regional Ocean COmmunity model, illustrates that the Moroccan slope is conducive to reflection of incident&#xd;
solitary waves of amplitude observed in the Strait of Gibraltar. A clear signature of these waves in the Tarifa&#xd;
high‐frequency sea level oscillations is depicted that paves the way to studies of the seasonality of ISWs in the&#xd;
Strait of Gibraltar with the long‐time series of sea level at Tarifa. The polarity of the reflected waves, observed&#xd;
with Acoustic Doppler Current Profilers/Conductivity‐Temperature‐Depth array moorings, presents a slight&#xd;
variability possibly due to the internal tide oscillations. The reflected ISWs arrives at the mooring location in&#xd;
phase with the peak of the internal tide. For the strongest tide, the pynocline approaches a critical point where the&#xd;
polarity of the ISWs might reverse.</dc:description>
      <dc:date>2024-12-03T08:23:34Z</dc:date>
      <dc:date>2024-12-03T08:23:34Z</dc:date>
      <dc:date>2024</dc:date>
      <dc:date>2024-02-05</dc:date>
      <dc:type>journal article</dc:type>
      <dc:identifier>Roustan, J.‐B., Bordois, L., García‐ Lafuente, J., Dumas, F., Auclair, F., &amp; Carton, X. (2024). Evidence of reflected internal solitary waves in the Strait of Gibraltar. Journal of Geophysical Research: Oceans, 129, e2023JC020152.</dc:identifier>
      <dc:identifier>https://hdl.handle.net/10630/35451</dc:identifier>
      <dc:identifier>10.1029/2023JC020152</dc:identifier>
      <dc:language>eng</dc:language>
      <dc:rights>http://creativecommons.org/licenses/by-nc/4.0/</dc:rights>
      <dc:rights>open access</dc:rights>
      <dc:rights>Attribution-NonCommercial 4.0 Internacional</dc:rights>
      <dc:publisher>American Geophysical Union</dc:publisher>
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