Carbon sequestration by mineral surface area as a feedback to climate warming in a greenhouse ocean. The project will investigate a previously unrecognised negative feedback to global warming resulting from sequestration of carbon to marine sediments by soil-formed clay minerals. By studying the past transitions to greenhouse periods, this project will assess the likely influence of this feedback in the present transition to a warmer climate.
What caused abrupt climate change events in the past and what can they tell us about the future? This project will improve our understanding of abrupt climate change in the past, present and future. It will dramatically enhance Australia's capacity to use climate models to assess the probability and associated consequences of abrupt climate change in the future.
Discovery Early Career Researcher Award - Grant ID: DE120102927
Funder
Australian Research Council
Funding Amount
$375,000.00
Summary
Ingredients of the eddy soup in Southern Ocean dynamics: processes, climate impacts and parameterisation. This project aims to understand jet-topography-eddy interactions in the Southern Ocean, and to apply that understanding to improving the representation of ocean physics in models. It will provide the underpinning science needed to increase confidence in climate predictions that will allow Australia to more effectively respond to climate change.
How will climate change affect sub-daily precipitation? This project will examine changes in sub-daily precipitation due to climate change. It will improve our understanding of the mechanisms that cause the changes at regional and local scales. Regional climate change projections produced will be freely available, and at a spatial and temporal scales suitable for impacts and adaptation studies.
Discovery Early Career Researcher Award - Grant ID: DE170100367
Funder
Australian Research Council
Funding Amount
$342,924.00
Summary
Decadal climate variability: Mechanisms, interactions and effects. This project aims to study the processes underlying decadal climate variability, through increasingly complex models, underpinned by observations. Climate variations on time scales of years, decades and longer affect Australia, with potentially devastating effects on agriculture, water supply, bushfires and health. Improved climate prediction on decadal time scales is urgently needed, but limited understanding of the system’s nat ....Decadal climate variability: Mechanisms, interactions and effects. This project aims to study the processes underlying decadal climate variability, through increasingly complex models, underpinned by observations. Climate variations on time scales of years, decades and longer affect Australia, with potentially devastating effects on agriculture, water supply, bushfires and health. Improved climate prediction on decadal time scales is urgently needed, but limited understanding of the system’s natural variability hampers progress. This knowledge will reduce uncertainty in near term climate projections, allowing more informed decision making about adaptation on the regional scale, particularly for sectors such as agriculture, health, water and ecosystem management (including bushfire control).Read moreRead less
Linkage Infrastructure, Equipment And Facilities - Grant ID: LE120100180
Funder
Australian Research Council
Funding Amount
$150,000.00
Summary
An Australian fluid-inclusion facility for climate-change science. Understanding past temperature and rainfall changes is essential for improving climate projections. The proposed facility will generate new palaeotemperature and palaeorainfall information from cave deposits, leading to a better understanding of natural climate variability and change.
Beyond the linear dynamics of the El Nino Southern Oscillation. This project will pioneer new climate models of the El Nino natural mode of climate variability, which will ultimately enable us to better predict seasonal weather fluctuation for Australia and improve our understanding of climate change in the tropical regions.
Interactions of physical processes for Southern Ocean dynamics. The Southern Ocean circulation is a major component of the earth’s climate system. Its behaviour depends strongly on the interactions of physical processes that are poorly understood and are not well represented in ocean models. This project will use laboratory experiments and fully-resolved flow simulations with appropriate scaling to examine the dynamics of key interactions between convection, mixing, wind-driven flow, eddies and ....Interactions of physical processes for Southern Ocean dynamics. The Southern Ocean circulation is a major component of the earth’s climate system. Its behaviour depends strongly on the interactions of physical processes that are poorly understood and are not well represented in ocean models. This project will use laboratory experiments and fully-resolved flow simulations with appropriate scaling to examine the dynamics of key interactions between convection, mixing, wind-driven flow, eddies and large-scale currents, while translating the results to improve ocean models. The project will develop the fundamental physics of the deep overturning circulation, the Antarctic Circumpolar Current, response timescales and heat uptake in a warming world, and improve predictions of oceanic and climate change.Read moreRead less
Melting and circulation in Antarctic ice shelf cavities. This project will explore and model the mechanisms causing the observed increased rate of melting of Antarctica’s ice shelves. This understanding is essential for accurate predictions of sea level rise and global thermohaline circulation over the next century, so that their impact on society can be planned for and mitigated.
A new energy budget for the global circulation of the oceans. The energy sources and sinks that govern the global circulation of the oceans will be re-evaluated, building a new picture of the energy budget of the oceans. This will lead to new knowledge of the circulation of the deep oceans, to better ocean and climate-prediction models, and ultimately to more reliable estimates of future climate change.