Stable doubly diffusive convectons
Dr Cedric Beaume (SOM), Prof Alastair Rucklidge (SoM)Contact email: email@example.com
Doubly diffusive convection is frequently encountered in natural sciences. For example, solar radiations heat the oceans making their surface warmer than their depth. In addition, due to evaporation, the density of salt in the oceans (salinity) increases towards the surface. This doubly diffusive convection configuration where salinity and temperature diffuse in the ocean is called thermohaline convection and gives rise to interesting phenomena. Indeed, the oceans are structured into thermohaline staircases in which the salinity remains mostly constant but jumps at specific depth levels. Thermohaline convection in these staircases is responsible for an instability called salt finger instability whereby the interface between two layers of different salinities becomes unstable and produces vertically elongated structures (fingers) of salty fluid sinking within the purer layer. This instability has been widely studied: it was found to play a major role in the mixing of the oceans at low latitude and to strongly interact with large scale oceanic currents.
In this project, we will investigate the properties of spatially localised doubly diffusive convection states named convectons. These states consist in one or few convection rolls surrounded by motionless fluid and persist in spite of the fact that the fluid is homogeneously forced. Convectons have recently been studied and revealed interesting properties among which: (i) they are linked to a phenomen called snaking, implying that a large number of them co-exist provided the same physical conditions and (ii) they are subcritical and associated to non trivial transitions past the instability threshold.
We will study the role of such states on the global dynamics of the doubly diffusive convection system. To that aim, we will consider different configurations to find stable convectons. These will constitute the first ever computation of stable spatially localised fluid flows in three dimensions. The characterisation of these convectons will provide invaluable information on their role in the typically chaotic dynamics observed in nature and advance the theory of pattern formation.
The student will study spatially localised states of doubly diffusive convection, namely convectons, in three dimensions. Important tasks will be undertaken to characterise their stability:
Stable convectons: the student will compute stable convectons in an elongated closed container. These solutions have always been found unstable due to an instability called twist instability. Computing stable convectons will be achieved by varying the size of the cross section of the closed container. This is guaranteed to work as two-dimensional computations revealed stable convectons and the absence of twist instability.
Convecton cartology: after stable convectons have been found, the student will work on a map showing where these convectons are stable as a function of the various parameters of the system. This will provide a better understanding on pattern formation in high dimensions and guide the design of experiments.
Onset of chaos: the mechanisms leading to chaos in doubly diffusive convection are not understood yet but stem from the emergence of convectons and of the twist instability. By choosing parameter values close to the twist instability threshold, the student will obtain invaluable information on the emergence of chaos in the hope of providing understanding on the structure of oubly diffusive chaos.
The student will work under the supervision of Dr C´edric Beaume and Prof Alastair Rucklidge within he Department of Applied Mathematics. This project provides a high level of specialist scientific raining in: (i) fluid dynamics, in particular in coupled convection problems; (ii) dynamical systems and more specifically in spatially localised pattern formation and (iii) high-performance computing with the handling of large scale simulations and data related to fluid flows. Co-supervision ill involve weekly formal meetings with Dr Beaume and Prof Rucklidge as well as more frequent eetings with Dr Beaume and/or Prof Rucklidge when necessary. An extended visit to the University of Toulouse (France) in Prof Alain Bergeon’s group will also be planned during the end of the second year. Prof Alain Bergeon is a collaborator of Dr Beaume and leading author on convectons. Dr Beaume and Prof Bergeon have already applied for a PICS collaborative grant from CNRS (http://www.cnrs.fr/derci/spip.php?article51) to fund travels and are awaiting results. In addition, the School of Mathematics at the University of Leeds would complement that fund and provide the student with a budget for research expenses. The PhD student will have access to a broad spectrum of training workshops put on by the Staff and Departmental development Unit at the University of Leeds and will also be provided with dedicated training on fluid dynamics and numerical methods by Dr Beaume and pattern formation by Prof Rucklidge.
The student should have a strong background in fluid dynamics and dynamical systems. They should have a taste for mathematics and numerics with a deep curiosity combined with an intense motivation.
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Related undergraduate subjects:
- Mechanical engineering