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  <abstract type="Summary">Theory and numerical simulations suggested that submesoscale fronts and filaments are subject to various types of instabilities, providing a potentially important pathway for the downscale transport and dissipation of mesoscale kinetic energy in the ocean. Based on the observational data collected from the Benguela upwelling system, this thesis, for the first time, provided direct evidence for the detailed structure of turbulence triggered by forced/unforced/inertial symmetric instability and marginal shear instability in submesoscale fronts.&lt;eng&gt;</abstract>
  <abstract type="Summary">Theorie und numerische Simulationen legten nahe, dass submesoskalige Fronten und Filamente verschiedenen Arten von Instabilitäten unterliegen, die einen potenziell wichtigen Weg für den abwärts gerichteten Transport und die Dissipation von mesoskaliger kinetischer Energie im Ozean darstellen. Basierend auf den Beobachtungsdaten, die im Benguela-Auftriebssystem gesammelt wurden, lieferte diese Arbeit zum ersten Mal direkte Beweise für die detaillierte Struktur der Turbulenz, die durch eine Vielzahl von submesoskaligen Instabilitäten in submesoskaligen Fronten ausgelöst wird.&lt;ger&gt;</abstract>
  <note type="statement of responsibility">vorgelegt von Jen-Ping Peng</note>
  <note>GutachterInnen: Lars Umlauf (Leibniz-Institut für Ostseeforschung Warnemünde) ; Bill Smyth (Oregon State University, USA)</note>
  <note type="thesis">Dissertation Universität Rostock 2020</note>
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      <title>Frontal instability and energy dissipation in submesoscale fronts</title>
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