Asymmetric vertical transport in weakly forced shallow flows
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arXiv
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| Format: | Preprint |
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2024
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| _version_ | 1866929303692771328 |
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| author | Ramírez, Lenin M. Flores Kamp, Leon P. J. Clercx, Herman J. H. Duran-Matute, Matias |
| author_facet | Ramírez, Lenin M. Flores Kamp, Leon P. J. Clercx, Herman J. H. Duran-Matute, Matias |
| contents | We report on an investigation of the vertical transport of tracer particles released within a shallow, continuously-forced flow by means of numerical simulations. The investigation is motivated by the shallow flows encountered in many environmental situations and inspired by the laboratory experiments conducted in electromagnetically forced shallow fluid layers. The flow is confined to a thin fluid layer by stress-free top and no-slip bottom walls. The dynamics and the transport properties of the shallow flow are investigated under various flow conditions characterized by a Reynolds number related to the forcing, $Re_F$, and the aspect ratio of vertical and horizontal length scales $δ$. The simulated shallow flows exhibit distinctive spatial distributions of vertical velocities: broader, weaker upwellings surrounded by narrower, stronger downwellings. These vertical flows are related to the horizontal flow structures, with updrafts occurring where the horizontal flow is vorticity-dominated, and the downdrafts where it is strain-dominated. The magnitude of the asymmetry in strength and size of the vertical flows and their correlation with horizontal structures depends on the flow conditions and significantly influences the vertical spreading of particles within the fluid volume. Under conditions leading to a large asymmetry, particles within updrafts are transported slowly upwards, while particles within downdrafts rapidly move downwards. In addition, particles are trapped for longer within the updrafts than downdrafts because of their correlation with vorticity-dominated regions. However, when the flow becomes fully three-dimensional and highly unsteady, this transport asymmetry subsides because the updrafts and downdrafts exhibit similar strength and size in such flow conditions. Consequently, similar amounts of particles are transported upwards and downwards at similar rates. |
| format | Preprint |
| id |
arxiv_https___arxiv_org_abs_2404_03807 |
| institution | arXiv |
| publishDate | 2024 |
| record_format | arxiv |
| spellingShingle | Asymmetric vertical transport in weakly forced shallow flows Ramírez, Lenin M. Flores Kamp, Leon P. J. Clercx, Herman J. H. Duran-Matute, Matias Fluid Dynamics We report on an investigation of the vertical transport of tracer particles released within a shallow, continuously-forced flow by means of numerical simulations. The investigation is motivated by the shallow flows encountered in many environmental situations and inspired by the laboratory experiments conducted in electromagnetically forced shallow fluid layers. The flow is confined to a thin fluid layer by stress-free top and no-slip bottom walls. The dynamics and the transport properties of the shallow flow are investigated under various flow conditions characterized by a Reynolds number related to the forcing, $Re_F$, and the aspect ratio of vertical and horizontal length scales $δ$. The simulated shallow flows exhibit distinctive spatial distributions of vertical velocities: broader, weaker upwellings surrounded by narrower, stronger downwellings. These vertical flows are related to the horizontal flow structures, with updrafts occurring where the horizontal flow is vorticity-dominated, and the downdrafts where it is strain-dominated. The magnitude of the asymmetry in strength and size of the vertical flows and their correlation with horizontal structures depends on the flow conditions and significantly influences the vertical spreading of particles within the fluid volume. Under conditions leading to a large asymmetry, particles within updrafts are transported slowly upwards, while particles within downdrafts rapidly move downwards. In addition, particles are trapped for longer within the updrafts than downdrafts because of their correlation with vorticity-dominated regions. However, when the flow becomes fully three-dimensional and highly unsteady, this transport asymmetry subsides because the updrafts and downdrafts exhibit similar strength and size in such flow conditions. Consequently, similar amounts of particles are transported upwards and downwards at similar rates. |
| title | Asymmetric vertical transport in weakly forced shallow flows |
| topic | Fluid Dynamics |
| url | https://arxiv.org/abs/2404.03807 |