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1 · Sources of anisotropy in the Reynolds stress tensor in the Stable
2 · Sources of anisotropy in the Reynolds stress tensor in the
3 · Quarterly Journal of the Royal Meteorological Society
4 · Lorenzo Giovannini
5 · Federica Faccini
6 · Energy cascade for highly anisotropic turbulence in the
7 · Dino
8 · Abstract EGU24

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N. Vercauteren and F. Gucci thank the University of Oslo for starter pack funds that covered part of the work. F. Gucci also thanks the University of Trento for supporting funds to spend a research period at the .

By studying the invariants of the anisotropy Reynolds stress tensor, it is possible to analyse the eddy kinetic energy distribution over the three components of the flow. Recent .Federica Gucci et al.,,,,, 1 Institute of Geophysics and Meteorology, University of Cologne, Köln, Germany ([email protected]) 2 Department of Civil, Environmental and Mechanical .F. Gucci, Department of Civil, Environmental and Mechanical Engineering, University of Trento, Trento 38122, Italy. Email: [email protected]. N. Vercauteren, Department of .

Vedi il profilo di Federica Faccini su LinkedIn, una community professionale di 1 miliardo di utenti.Federica Gucci, "High-resolution simulations of the thermally-driven valley-exit jet of the Isarco Valley", Academic Year 2017/2018, Master Degree in Physics, University of Trento. PhD Previous studies have demonstrated that stably stratified turbulence still has a forward energy cascade, rather than an inverse energy cascade (Gucci et al., 2023; Sozza et .University of Trento: Trento, Trentino Alto Adige, IT . Professor (Department of Civil, Environmental and Mechanical Engineering) Employment Show more detail . Contributors: .

Abstract. Data collected by 12 sonic anemometers over the Plaine Morte Glacier (Swiss Alps) during the Snow Horizontal Arrays Turbulence Study are used to investigate sources of anisotropy in the Reynolds stress tensor for .Quarterly Journal of the Royal Meteorological Society. 2023-01 | Journal article. DOI: 10.1002/qj.4407. Contributors: Federica Gucci; Lorenzo Giovannini; Ivana Stiperski; Dino . N. Vercauteren and F. Gucci thank the University of Oslo for starter pack funds that covered part of the work. F. Gucci also thanks the University of Trento for supporting funds to spend a research period at the Freie Universität Berlin, where part of the work has been done.

By studying the invariants of the anisotropy Reynolds stress tensor, it is possible to analyse the eddy kinetic energy distribution over the three components of the flow. Recent analyses of SBL turbulence data highlighted a prevalence of .Federica Gucci et al.,,,,, 1 Institute of Geophysics and Meteorology, University of Cologne, Köln, Germany ([email protected]) 2 Department of Civil, Environmental and Mechanical Engineering, University of Trento, Trento, ItalyF. Gucci, Department of Civil, Environmental and Mechanical Engineering, University of Trento, Trento 38122, Italy. Email: [email protected]. N. Vercauteren, Department of Geosciences, University of Oslo, Oslo, Norway. Email: [email protected]. 1 INTRODUCTION Ivana Stiperski2. Dino Zardi1. Abstract.Vedi il profilo di Federica Faccini su LinkedIn, una community professionale di 1 miliardo di utenti.

Federica Gucci, "High-resolution simulations of the thermally-driven valley-exit jet of the Isarco Valley", Academic Year 2017/2018, Master Degree in Physics, University of Trento. PhD

Previous studies have demonstrated that stably stratified turbulence still has a forward energy cascade, rather than an inverse energy cascade (Gucci et al., 2023; Sozza et al., 2015). Thus, it.University of Trento: Trento, Trentino Alto Adige, IT . Professor (Department of Civil, Environmental and Mechanical Engineering) Employment Show more detail . Contributors: Federica Gucci; Lorenzo Giovannini; Ivana Stiperski; Dino Zardi; Nikki Vercauteren Show more detail. Source: check . Abstract. Data collected by 12 sonic anemometers over the Plaine Morte Glacier (Swiss Alps) during the Snow Horizontal Arrays Turbulence Study are used to investigate sources of anisotropy in the Reynolds stress tensor for stable boundary layers.

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Quarterly Journal of the Royal Meteorological Society. 2023-01 | Journal article. DOI: 10.1002/qj.4407. Contributors: Federica Gucci; Lorenzo Giovannini; Ivana Stiperski; Dino Zardi; Nikki Vercauteren. N. Vercauteren and F. Gucci thank the University of Oslo for starter pack funds that covered part of the work. F. Gucci also thanks the University of Trento for supporting funds to spend a research period at the Freie Universität Berlin, where part of the work has been done.

By studying the invariants of the anisotropy Reynolds stress tensor, it is possible to analyse the eddy kinetic energy distribution over the three components of the flow. Recent analyses of SBL turbulence data highlighted a prevalence of .

Federica Gucci et al.,,,,, 1 Institute of Geophysics and Meteorology, University of Cologne, Köln, Germany ([email protected]) 2 Department of Civil, Environmental and Mechanical Engineering, University of Trento, Trento, ItalyF. Gucci, Department of Civil, Environmental and Mechanical Engineering, University of Trento, Trento 38122, Italy. Email: [email protected]. N. Vercauteren, Department of Geosciences, University of Oslo, Oslo, Norway. Email: [email protected]. 1 INTRODUCTION Ivana Stiperski2. Dino Zardi1. Abstract.Vedi il profilo di Federica Faccini su LinkedIn, una community professionale di 1 miliardo di utenti.

Federica Gucci, "High-resolution simulations of the thermally-driven valley-exit jet of the Isarco Valley", Academic Year 2017/2018, Master Degree in Physics, University of Trento. PhD Previous studies have demonstrated that stably stratified turbulence still has a forward energy cascade, rather than an inverse energy cascade (Gucci et al., 2023; Sozza et al., 2015). Thus, it.University of Trento: Trento, Trentino Alto Adige, IT . Professor (Department of Civil, Environmental and Mechanical Engineering) Employment Show more detail . Contributors: Federica Gucci; Lorenzo Giovannini; Ivana Stiperski; Dino Zardi; Nikki Vercauteren Show more detail. Source: check .

Abstract. Data collected by 12 sonic anemometers over the Plaine Morte Glacier (Swiss Alps) during the Snow Horizontal Arrays Turbulence Study are used to investigate sources of anisotropy in the Reynolds stress tensor for stable boundary layers.

Sources of anisotropy in the Reynolds stress tensor in the Stable

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Sources of anisotropy in the Reynolds stress tensor in the Stable

Sources of anisotropy in the Reynolds stress tensor in the

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