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Quantifying variability in Lagrangian particle dispersal in ocean ensemble simulations: an information theory approach

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  • Additional Information
    • Contributors:
      Helmholtz Centre for Ocean Research Kiel (GEOMAR); Institut Mediterrani d'Estudis Avancats = Instituto Mediterráneo de Estudios Avanzados (IMEDEA); Consejo Superior de Investigaciones Cientificas España = Spanish National Research Council Spain (CSIC)-Universitat de les Illes Balears = Universidad de las Islas Baleares = University of the Balearic Islands (UIB); Debye Institute for Nanomaterials Science; Universiteit Utrecht / Utrecht University Utrecht; Institut des Géosciences de l’Environnement (IGE); Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Observatoire des Sciences de l'Univers de Grenoble (Fédération OSUG)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP); Université Grenoble Alpes (UGA); Institute for Marine and Atmospheric Research Utrecht (IMAU); ANR-13-BS06-0007,OCCIPUT,Chaos océanique – Impacts, structure, prévisibilité(2013)
    • Publication Information:
      CCSD
      European Geosciences Union (EGU)
    • Publication Date:
      2025
    • Collection:
      Université Grenoble Alpes: HAL
    • Abstract:
      International audience ; Ensemble Lagrangian simulations aim to capture the full range of possible outcomes for particle dispersal. However, single-member Lagrangian simulations are most commonly available and only provide a subset of the possible particle dispersal outcomes. This study explores how to generate the variability inherent in Lagrangian ensemble simulations by creating variability in a single-member simulation. To obtain a reference for comparison, we performed ensemble Lagrangian simulations by advecting the particles from the surface of the Gulf Stream, around 35.61° N, 73.61° W, in each member to obtain trajectories capturing the variability of the full 50-member ensemble. Subsequently, we performed single-member simulations with spatially and temporally varying release strategies to generate comparable trajectory variability and dispersal and also with adding Brownian motion diffusion to the advection. We studied how these strategies affected the number of surface particles connecting the Gulf Stream with the eastern side of the subtropical gyre. We used an information theory approach to define and compare the variability in the ensemble with the single-member strategies. We defined the variability as the marginal entropy or average information content of the probability distributions of the position of the particles. We calculated the relative entropy to quantify the uncertainty of representing the full-ensemble variability with single-member simulations. We found that release periods of 12 to 20 weeks most effectively captured the full ensemble variability, while spatial releases with a 2.0° radius resulted in the closest match at timescales shorter than 10 d. We found that adding relatively high amounts of Brownian motion diffusion ( K h = 1000 m 2 s −1 ) captures the entropy aspects of the full ensemble variability well but leads to an overestimation of connectivity. Our findings provide insights to improve the representation of variability in particle trajectories and define a framework for ...
    • Relation:
      WOS: 001596350300001
    • Accession Number:
      10.5194/npg-32-411-2025
    • Online Access:
      https://hal.science/hal-05384755
      https://hal.science/hal-05384755v1/document
      https://hal.science/hal-05384755v1/file/Pierard2025.pdf
      https://doi.org/10.5194/npg-32-411-2025
    • Rights:
      https://creativecommons.org/licenses/by/4.0/ ; info:eu-repo/semantics/OpenAccess
    • Accession Number:
      edsbas.78A8B48E