Linkage Infrastructure, Equipment And Facilities - Grant ID: LE180100166
Funder
Australian Research Council
Funding Amount
$637,800.00
Summary
Four-dimensional coherent imaging velocimetry facility for fluid mechanics research. This project aims to enhance understanding of multi-scale fluid flows in engineering, geophysics and biomedicine by delivering a facility for high temporal and spatial resolution, three-dimensional velocity measurements. The four-dimensional, coherent imaging velocimetry facility for fluid mechanics research is aimed at addressing limitations of commercially available imaging systems. It is expected to provide ....Four-dimensional coherent imaging velocimetry facility for fluid mechanics research. This project aims to enhance understanding of multi-scale fluid flows in engineering, geophysics and biomedicine by delivering a facility for high temporal and spatial resolution, three-dimensional velocity measurements. The four-dimensional, coherent imaging velocimetry facility for fluid mechanics research is aimed at addressing limitations of commercially available imaging systems. It is expected to provide unprecedented measurement capabilities with significant benefit to the design, control and modelling of complex fluid flows found in many areas. Applications include the jets used for heating, cooling, mixing, and drug delivery in engineering and pharmacy to the kinematics of sperm and micro-organisms in bio-medicine, and wave-particle flows in geo-physics.Read moreRead less
The fluid dynamics of intrusions. This project aims to investigate intrusions, the primarily horizontal flows of well-mixed fluid into density-stratified surroundings. Such flows are fundamental in the atmosphere and oceans, but they are little understood because they are controlled by strong feedback between the intrusion and internal waves generated in the stratified ambient. Existing studies rely on computationally intensive simulations, analogue experiments or ad-hoc models of limited appl ....The fluid dynamics of intrusions. This project aims to investigate intrusions, the primarily horizontal flows of well-mixed fluid into density-stratified surroundings. Such flows are fundamental in the atmosphere and oceans, but they are little understood because they are controlled by strong feedback between the intrusion and internal waves generated in the stratified ambient. Existing studies rely on computationally intensive simulations, analogue experiments or ad-hoc models of limited applicability. This project expects to develop and validate a new, broadly applicable and rigorous mathematical model for such flows. Expected benefits include improved volcanic ash dispersal modelling and improved understanding of climate-critical oceanic and atmospheric flows.Read moreRead less
Dynamics of fire whirls and dust devils. The project aims to develop fundamental understanding and models to inform the development of more accurate computer models of fire front propagation. Fire whirls and dust devils are strongly swirling localised vortex flows that result from an interplay of circulation and buoyancy, may extend hundreds of metres into the air. By projecting firebrands well away from the ground strike, fire whirls can initiate spot fires well beyond a fire front, advancing f ....Dynamics of fire whirls and dust devils. The project aims to develop fundamental understanding and models to inform the development of more accurate computer models of fire front propagation. Fire whirls and dust devils are strongly swirling localised vortex flows that result from an interplay of circulation and buoyancy, may extend hundreds of metres into the air. By projecting firebrands well away from the ground strike, fire whirls can initiate spot fires well beyond a fire front, advancing fronts at much higher speeds than most fire spread models predict. The project aims to improve understanding of the sets of local conditions that produce and stabilise these flows, using computational fluid dynamics matched to laboratory experiments and dimensional analysis of results.Read moreRead less
The Cenozoic tectonic evolution of East and Southeast Asia: interplay between the India-Eurasia collision and the Pacific and Sunda subduction zones. This project investigates how the Indo-Australian and Pacific tectonic plates have interacted with the Eurasian plate to form the largest continental deformation zone on Earth in East Asia, stretching from the Himalayas to Indonesia and eastern Siberia. This is important for understanding how mountain ranges form and how continents are torn apart.
Discovery Early Career Researcher Award - Grant ID: DE150100326
Funder
Australian Research Council
Funding Amount
$338,266.00
Summary
The role of subduction initiation in the evolution of Earth’s oceans. An outstanding question in plate tectonics is how do oceans start to close? The Wilson Cycle describes the life of an ocean in three phases: opening and spreading, foundering of its passive margins and development of new subduction zones, and consumption and closure. It has been suggested that new subduction zones are difficult to form and thereby they are more likely to spread from ocean to ocean like a sort of invasive mecha ....The role of subduction initiation in the evolution of Earth’s oceans. An outstanding question in plate tectonics is how do oceans start to close? The Wilson Cycle describes the life of an ocean in three phases: opening and spreading, foundering of its passive margins and development of new subduction zones, and consumption and closure. It has been suggested that new subduction zones are difficult to form and thereby they are more likely to spread from ocean to ocean like a sort of invasive mechanism. This project aims to make use of laboratory models and plate kinematic modelling to understand how subduction zones are initiating and propagating in the Atlantic. The project aims to provide clues on how ancient oceans may have closed and whether the Atlantic is already in its turning point.Read moreRead less
Intraplate volcanism near lateral slab edges: result of deep mantle plumes or slab rollback-induced mantle flow? This project investigates how the Earth's interior (the mantle) flows near edges of tectonic plates as these plates sink into the mantle. This is important because these flows have been crucial in shaping the Southwest Pacific region bordering Australia and might be responsible for the formation of some of the largest volcanoes on Earth.
Discovery Early Career Researcher Award - Grant ID: DE210100004
Funder
Australian Research Council
Funding Amount
$440,185.00
Summary
Mixing and air-sea coupling in the Pacific: Toward better El Nino forecasts. The Tropical Pacific drives significant year-to-year variability in Australian rainfall and climate extremes. However, tropical climate predictions are severely limited due to systematic biases in numerical climate models. Using new techniques and leveraging international collaborations, this project aims to transform our ability to simulate tropical Pacific climate through a new understanding of key air-sea interaction ....Mixing and air-sea coupling in the Pacific: Toward better El Nino forecasts. The Tropical Pacific drives significant year-to-year variability in Australian rainfall and climate extremes. However, tropical climate predictions are severely limited due to systematic biases in numerical climate models. Using new techniques and leveraging international collaborations, this project aims to transform our ability to simulate tropical Pacific climate through a new understanding of key air-sea interaction and ocean mixing processes. Expected outcomes include a better representation of tropical climate in the Australian climate model and improved seasonal to interannual predictive capability. These improved predictions will give communities more time to prepare for extreme events such as droughts, heatwaves and bushfires.Read moreRead less
Three-dimensional subduction models of overriding plate deformation and mantle flow using laboratory and numerical methods. This project investigates the interaction of the Earth's tectonic plates at subduction zones, places where one plate sinks below another plate into the Earth. This is important for understanding the evolution of the Australian plate that has active subduction zones to the north and east, and how its geological evolution is controlled by subduction.
Discovery Early Career Researcher Award - Grant ID: DE220101027
Funder
Australian Research Council
Funding Amount
$455,906.00
Summary
Resolving ocean convection: new knowledge for a changing Antarctica. This project aims to improve our understanding of the role of convection on the Antarctic margins using a high-resolution, cutting-edge numerical approach. Convection is an important, but poorly understood oceanic process, which diverts heat away from the melting Antarctic ice shelves by transporting cold and salty water from the ocean surface to depth. The project outcomes will be new knowledge of the physics from novel numeri ....Resolving ocean convection: new knowledge for a changing Antarctica. This project aims to improve our understanding of the role of convection on the Antarctic margins using a high-resolution, cutting-edge numerical approach. Convection is an important, but poorly understood oceanic process, which diverts heat away from the melting Antarctic ice shelves by transporting cold and salty water from the ocean surface to depth. The project outcomes will be new knowledge of the physics from novel numerical models and theory, supported by insights from observations and model parameterisations. This timely research will improve prediction of sea level rise due to a changing Antarctica and enhance our ability to adapt to future climate scenarios, providing significant environmental and health benefits to Australians.Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE110100094
Funder
Australian Research Council
Funding Amount
$300,000.00
Summary
Selective laser melting - an advanced manufacturing and physical modelling technology for the digital age. Selective laser melting is a new manufacturing technology that creates parts layer by layer directly from a computer model, eliminating the need for tooling or machining. This technology will be applied to a diverse range of research areas from producing the next generation of medical implants and devices to improving our understanding of geo-materials.