Large Scale Natural Convection Boundary Layers with Non-Boussinesq Effects. This proposal aims to understand and predict heat transfer by turbulent natural convection in two scenarios, firstly at very large environmental scales, such as occur on melting Antarctic ice sheets, and secondly convection involving very large temperature differences such as occur in solar thermal power plants and industrial processes. These natural convection flow regimes are incredibly difficult to investigate directl ....Large Scale Natural Convection Boundary Layers with Non-Boussinesq Effects. This proposal aims to understand and predict heat transfer by turbulent natural convection in two scenarios, firstly at very large environmental scales, such as occur on melting Antarctic ice sheets, and secondly convection involving very large temperature differences such as occur in solar thermal power plants and industrial processes. These natural convection flow regimes are incredibly difficult to investigate directly but by focusing on the fundamental dynamics of the turbulent flows using large scale numerical simulations and innovative experiments, the project is expected to develop better analytical and computational models which will underpin improvements in
global ocean models and improve energy efficiency.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE110100079
Funder
Australian Research Council
Funding Amount
$500,000.00
Summary
Experimental facility for extreme air/sea interaction studies. The level of greenhouse gases in the atmosphere which cause global warming is greatly influenced by interactions at the air/sea interface. This infrastructure will allow in-depth studies of these interactions and contribute to much improved strategies to control greenhouse gases.
Discovery Early Career Researcher Award - Grant ID: DE150100985
Funder
Australian Research Council
Funding Amount
$390,000.00
Summary
Entrainment and interface dynamics of turbulent flows. Patches of turbulent flow such as in clouds, volcanic or bushfire plumes grow with time because they draw or entrain non-turbulent fluid through their boundaries. The quantity of fluid entrained, and why it entrains this amount, is poorly understood. This is a major bottleneck in our ability to predict how these natural phenomena evolve in time. This project aims to employ idealised laboratory models of these natural phenomena, and utilise h ....Entrainment and interface dynamics of turbulent flows. Patches of turbulent flow such as in clouds, volcanic or bushfire plumes grow with time because they draw or entrain non-turbulent fluid through their boundaries. The quantity of fluid entrained, and why it entrains this amount, is poorly understood. This is a major bottleneck in our ability to predict how these natural phenomena evolve in time. This project aims to employ idealised laboratory models of these natural phenomena, and utilise high quality measurement techniques and theoretical tools to quantify and understand the physical basis of the entrainment mechanism. The project aims to create better climate models and more accurate predictions of natural disasters associated with bushfires and volcanos.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE140100079
Funder
Australian Research Council
Funding Amount
$200,000.00
Summary
A thermally stratified Sea-Ice-Wave Interaction Facility. A thermally stratified sea ice wave interaction facility: Predictions of climate change now impact all levels of society as future political, social and environmental plans are made on the basis of these models. Predictions require models of many complex dynamical processes with a wide range of parameters. An important process is the Marginal Ice Zone (MIZ) dynamics. The MIZ is the region between the open ocean and the fully ice-covered o ....A thermally stratified Sea-Ice-Wave Interaction Facility. A thermally stratified sea ice wave interaction facility: Predictions of climate change now impact all levels of society as future political, social and environmental plans are made on the basis of these models. Predictions require models of many complex dynamical processes with a wide range of parameters. An important process is the Marginal Ice Zone (MIZ) dynamics. The MIZ is the region between the open ocean and the fully ice-covered ocean where waves and ice interact, causing ice-breaking and wave attenuation. This unique facility will enable experiments in sea-ice-wave interactions in a controlled environment. Water and air temperature, thermal stratification, water waveform and ice properties will be adjusted in order to preserve key characteristics of the complex ocean environment.Read moreRead less