Geophysical flows over topography, a playground for laboratory experiments

Physicists face major challenges in modelling multi-scale phenomena that are observed in geophysical flows (e.g. in the Earth’s oceans and atmosphere, or liquid planetary cores). In particular, complexities arise because geophysical fluids are rotating and subject to density variations, but also bec...

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Main Authors: Vidal, Jérémie, Noir, Jérôme, Cébron, David, Burmann, Fabian, Monville, Rémy, Giraud, Vadim, Charles, Yoann
Format: Article
Language:English
Published: Académie des sciences 2025-01-01
Series:Comptes Rendus. Physique
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Online Access:https://comptes-rendus.academie-sciences.fr/physique/articles/10.5802/crphys.219/
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author Vidal, Jérémie
Noir, Jérôme
Cébron, David
Burmann, Fabian
Monville, Rémy
Giraud, Vadim
Charles, Yoann
author_facet Vidal, Jérémie
Noir, Jérôme
Cébron, David
Burmann, Fabian
Monville, Rémy
Giraud, Vadim
Charles, Yoann
author_sort Vidal, Jérémie
collection DOAJ
description Physicists face major challenges in modelling multi-scale phenomena that are observed in geophysical flows (e.g. in the Earth’s oceans and atmosphere, or liquid planetary cores). In particular, complexities arise because geophysical fluids are rotating and subject to density variations, but also because the fluid boundaries have complex geometries (e.g. the ocean floor) with wavelengths ranging from metres to thousands of kilometres. Dynamical models of planetary fluid layers are thus often constrained by observations, whose interpretation necessitates a comprehensive understanding of the underlying physics. To this end, geophysical studies often combine cutting-edge experiments across a wide range of parameters, together with theory and numerical simulations, to derive predictive scaling laws applicable for planetary settings. In this review, we discuss experimental efforts that have contributed to our understanding of geophysical flows with topography. More specifically, we focus on (i) the flow response to mechanical (orbital) forcings in the presence of a large-scale (ellipsoidal) topography, (ii) some effects of small-scale topography onto bulk flows and boundary-layer dynamics, and (iii) the interaction between convection and roughness. The geophysical context is briefly introduced for each case, and some experimental perspectives are drawn.
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issn 1878-1535
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publishDate 2025-01-01
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series Comptes Rendus. Physique
spelling doaj-art-7c19ce89a75945559eae7fd9a0e002a52025-02-07T13:54:24ZengAcadémie des sciencesComptes Rendus. Physique1878-15352025-01-0115210.5802/crphys.21910.5802/crphys.219Geophysical flows over topography, a playground for laboratory experimentsVidal, Jérémie0https://orcid.org/0000-0002-3654-6633Noir, Jérôme1https://orcid.org/0000-0001-9977-0360Cébron, David2https://orcid.org/0000-0002-3579-8281Burmann, Fabian3https://orcid.org/0000-0001-8095-1081Monville, Rémy4https://orcid.org/0000-0002-9460-2293Giraud, Vadim5https://orcid.org/0009-0003-6820-0148Charles, Yoann6https://orcid.org/0000-0002-4861-8016Université Grenoble Alpes, CNRS, ISTerre, 38000 Grenoble, FranceInstitut für Geophysik, ETH Zürich, Sonneggstrasse 5, Zürich 8092, SwitzerlandUniversité Grenoble Alpes, CNRS, ISTerre, 38000 Grenoble, FranceInstitut für Geophysik, ETH Zürich, Sonneggstrasse 5, Zürich 8092, SwitzerlandUniversité Grenoble Alpes, CNRS, ISTerre, 38000 Grenoble, FranceInstitut für Geophysik, ETH Zürich, Sonneggstrasse 5, Zürich 8092, SwitzerlandDevelopment of Advanced Engineering Solutions (DAES), Avenue des Grandes-Communes 8, Petit-Lancy 1213, Switzerland; Institut für Geophysik, ETH Zürich, Sonneggstrasse 5, Zürich 8092, SwitzerlandPhysicists face major challenges in modelling multi-scale phenomena that are observed in geophysical flows (e.g. in the Earth’s oceans and atmosphere, or liquid planetary cores). In particular, complexities arise because geophysical fluids are rotating and subject to density variations, but also because the fluid boundaries have complex geometries (e.g. the ocean floor) with wavelengths ranging from metres to thousands of kilometres. Dynamical models of planetary fluid layers are thus often constrained by observations, whose interpretation necessitates a comprehensive understanding of the underlying physics. To this end, geophysical studies often combine cutting-edge experiments across a wide range of parameters, together with theory and numerical simulations, to derive predictive scaling laws applicable for planetary settings. In this review, we discuss experimental efforts that have contributed to our understanding of geophysical flows with topography. More specifically, we focus on (i) the flow response to mechanical (orbital) forcings in the presence of a large-scale (ellipsoidal) topography, (ii) some effects of small-scale topography onto bulk flows and boundary-layer dynamics, and (iii) the interaction between convection and roughness. The geophysical context is briefly introduced for each case, and some experimental perspectives are drawn.https://comptes-rendus.academie-sciences.fr/physique/articles/10.5802/crphys.219/TopographyRotationStratificationGeophysical flowsPlanetary coresSubsurface oceans
spellingShingle Vidal, Jérémie
Noir, Jérôme
Cébron, David
Burmann, Fabian
Monville, Rémy
Giraud, Vadim
Charles, Yoann
Geophysical flows over topography, a playground for laboratory experiments
Comptes Rendus. Physique
Topography
Rotation
Stratification
Geophysical flows
Planetary cores
Subsurface oceans
title Geophysical flows over topography, a playground for laboratory experiments
title_full Geophysical flows over topography, a playground for laboratory experiments
title_fullStr Geophysical flows over topography, a playground for laboratory experiments
title_full_unstemmed Geophysical flows over topography, a playground for laboratory experiments
title_short Geophysical flows over topography, a playground for laboratory experiments
title_sort geophysical flows over topography a playground for laboratory experiments
topic Topography
Rotation
Stratification
Geophysical flows
Planetary cores
Subsurface oceans
url https://comptes-rendus.academie-sciences.fr/physique/articles/10.5802/crphys.219/
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