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Bruno Blanke

Researcher at IFREMER

Publications -  85
Citations -  5077

Bruno Blanke is an academic researcher from IFREMER. The author has contributed to research in topics: Ocean current & Water mass. The author has an hindex of 34, co-authored 83 publications receiving 4475 citations. Previous affiliations of Bruno Blanke include University of California, Los Angeles & Centre national de la recherche scientifique.

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Variability of the Tropical Atlantic Ocean Simulated by a General Circulation Model with Two Different Mixed-Layer Physics

TL;DR: In this article, a 1.5 turbulence closure model in an ocean general circulation model of the equatorial Atlantic is presented, where the eddy viscosity and diffusivity involved in the vertical mixing are defined as the product of a characteristic turbulent velocity and a characteristic mixing length.
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Kinematics of the Pacific Equatorial Undercurrent: An Eulerian and Lagrangian Approach from GCM Results

TL;DR: In this paper, three-dimensional monthly velocity fields from an ocean general circulation model are used to study the annual mean mass balance of the Pacific Equatorial Undercurrent (EUC).
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Lagrangian ocean analysis: Fundamentals and practices

TL;DR: Lagrangian analysis is a powerful way to analyse the output of ocean circulation models and other ocean velocity data such as from altimetry as mentioned in this paper, where large sets of virtual particles are integrated within the 3D, time-evolving velocity fields.
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Short communication: A Lagrangian tool for modelling ichthyoplankton dynamics

TL;DR: Ichthyop is a free Java tool designed to study the effects of physical and biological factors on ichthyoplankton dynamics and generates output files that can be post-processed easily using graphic and statistical software.
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Warm water paths in the equatorial Atlantic as diagnosed with a general circulation model

TL;DR: In this article, the authors used a global ocean general circulation model to study the main circulation patterns within the upper 1200 m of the equatorial Atlantic, where they used Lagrangian techniques to picture and quantify the routes followed in the model by distinct water mass classes, defined by their initial temperature on model transatlantic sections at 10°S and 10°N.