Measurements in a turbulent patch in a rotating,linearly-stratified fluid |
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| Institution: | 1. Department of Civil Engineering, The University, Dundee DD1 4HN, UK;2. Environmental Fluid Dynamics Program, Department of Mechanical and Aerospace Engineering, Arizona State University, Tempe, AZ 85287-6106, USA;1. von Karman Institute for Fluid Dynamics, Waterloosesteenweg 72, Sint-Genesius-Rode, Belgium;2. Aerospace Engineering Group, Universidad Carlos III de Madrid, Av. de la Universidad 30, Leganés, Spain;3. Department of Aerospace Engineering, University of Bristol, University Walk, BS81TR Bristol, UK;1. Key Laboratory Equipment Design and Manufacturing Technology, School of Mechanical Engineering, Tianjin University, Tianjin 300054, China;2. School of Mechanical and Manufacturing Engineering, National University of Sciences and Technology, Islamabad 44000, Pakistan;3. Griffith School of Engineering, Gold Coast Campus, Griffith University, QLD 4222, Australia;1. Faculty of Aerospace Engineering, Alma Mater Studiorum – University of Bologna, Forlì, Italy;2. FLOW, Engineering Mechanics, KTH Royal Institute of Technology, Stockholm, Sweden;1. Laboratory of Mathematics and Complex Systems, School of Mathematical Sciences, Beijing Normal University, Beijing, China;2. Academy for Advanced Interdisciplinary Studies, Southern University of Science and Technology, Shenzhen, China |
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| Abstract: | A series of experiments is described in which a turbulent patch is generated locally by an oscillating grid positioned at one end and mid-depth of a rotating channel filled initially with a linearly-stratified fluid. Measurements have been made of vertical density profiles through the patch both during sustained oscillations and following cessation of grid forcing. Temporal variations in patch size and structure, Thorpe scales, mixedness parameter and available potential energy are deduced from these measurements, and the effects thereon of varying the background rotation rate, initial buoyancy frequency and grid action are investigated. For the growth phase of the patch, previous results obtained by other workers are confirmed and extended. Because the rapid turbulent motions implied a large Rossby number, rotation was not important during this phase. During the decay phase, rotational effects are shown to become important, and the presence of rotation is found to retard the decay of both the mixedness and the Thorpe scales of the density overturns within the patch. The work is novel in that measurements of the patch parameters listed above have not previously been carried out in the presence of rotation. The results are relevant to studies of such patches that have been observed in the ocean and atmosphere. |
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