Quantitative reconstructions of Australian climates since the last Interglacial. A crucial test of the models used to project future climate is how well they reproduce past climates. The project will reconstruct Australian regional climates, from vegetation, fire and runoff records, and use these for climate-model evaluation - helping to provide a more solid basis for management of Australian resources in the future.
The puzzle of landfast sea ice: ‘Fast’ ice and near-term climate impacts. Sea ice which is held motionless against the Antarctic coastline (so-called landfast, or 'fast' ice) is hugely important for global climate and Southern Ocean ecosystems but its extent has recently plummeted. This project will address major knowledge gaps by providing novel satellite-based mapping and analysis of fast ice extent, towards enabling incorporation of fast ice into Australia’s new sea ice-ocean Earth system mod ....The puzzle of landfast sea ice: ‘Fast’ ice and near-term climate impacts. Sea ice which is held motionless against the Antarctic coastline (so-called landfast, or 'fast' ice) is hugely important for global climate and Southern Ocean ecosystems but its extent has recently plummeted. This project will address major knowledge gaps by providing novel satellite-based mapping and analysis of fast ice extent, towards enabling incorporation of fast ice into Australia’s new sea ice-ocean Earth system model for the first time – to allow assessment of its impacts on global ocean circulation and ice shelf melt. Outcomes also include new automated capability for monitoring fast ice extent, analysis of its variability and drivers, and first maps of its thickness and roughness.Read moreRead less
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: DE210101433
Funder
Australian Research Council
Funding Amount
$429,043.00
Summary
From creeping to sliding: controls on Antarctic Ice Sheet flow processes. This project aims to provide new insight into how ice flow processes influence Antarctic ice loss - a serious unsolved problem in predicting how much Antarctica will contribute to sea level rise. Using a state-of-the-art ice sheet model and real-world glaciological observations, this project expects to generate new knowledge of the mechanisms, and environmental and climatic conditions that control ice flow. Expected outcom ....From creeping to sliding: controls on Antarctic Ice Sheet flow processes. This project aims to provide new insight into how ice flow processes influence Antarctic ice loss - a serious unsolved problem in predicting how much Antarctica will contribute to sea level rise. Using a state-of-the-art ice sheet model and real-world glaciological observations, this project expects to generate new knowledge of the mechanisms, and environmental and climatic conditions that control ice flow. Expected outcomes of this project are improved estimates of Antarctica’s contribution to future sea level rise. This project should provide substantial benefits in Australia and internationally, particularly in regions vulnerable to rising sea levels, by producing a sound evidence base for policy and mitigation strategies.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE150100223
Funder
Australian Research Council
Funding Amount
$357,024.00
Summary
Dynamics, variability and change in Southern Ocean abyssal flows. Changes in the Southern Ocean abyssal circulation are linked with dramatic climate events, yet the associated dynamics are poorly understood. This project aims to determine the fundamental dynamic processes driving abyssal flows, and diagnose impacts of recent and projected climate change. The project also aims to bridge the large gap between conceptual and observational understanding of this vital limb of the ocean's overturning ....Dynamics, variability and change in Southern Ocean abyssal flows. Changes in the Southern Ocean abyssal circulation are linked with dramatic climate events, yet the associated dynamics are poorly understood. This project aims to determine the fundamental dynamic processes driving abyssal flows, and diagnose impacts of recent and projected climate change. The project also aims to bridge the large gap between conceptual and observational understanding of this vital limb of the ocean's overturning circulation. A significant innovation is that it will be the first study of the Southern Ocean abyss using realistic global-scale models capable of simulating all the key dynamic processes. Results will guide Southern Ocean observation programs, explain observed changes, and reduce uncertainties in climate projections.Read moreRead less
Discovery Early Career Researcher Award - Grant ID: DE220100279
Funder
Australian Research Council
Funding Amount
$453,000.00
Summary
Did ocean circulation changes build the Antarctic ice sheet? The evolution of the Antarctic ice sheet, from its beginning 34 million years ago (Ma) until today, is critical to our understanding of future climate change. This project aims to improve climate and ocean model simulations of the early Oligocene (30 Ma) and middle Miocene (15 Ma), using higher resolution and more accurate paleogeography than has previously been done. Expected outcomes include improvements to paleoclimate reconstructio ....Did ocean circulation changes build the Antarctic ice sheet? The evolution of the Antarctic ice sheet, from its beginning 34 million years ago (Ma) until today, is critical to our understanding of future climate change. This project aims to improve climate and ocean model simulations of the early Oligocene (30 Ma) and middle Miocene (15 Ma), using higher resolution and more accurate paleogeography than has previously been done. Expected outcomes include improvements to paleoclimate reconstructions, better constraints on future climate change, and a better understanding of the impact of ocean eddies on Antarctic climate. These outcomes should strengthen Australia’s long-term program of climate modelling, and enable more effective climate adaptation, mitigation and risk management.Read moreRead less
The Southern Ocean's response to abrupt climate change. This project aims to determine how the Southern Ocean responds to abrupt climate change, through geochemical analysis of marine sediment cores. Rapid warming events of the last ice age provide an analogue to human-caused warming. Experiments using ocean climate models will evaluate the drivers and consequences of the biogeochemical response of different sectors and zones of the Southern Ocean. The intended outcome is a better understanding ....The Southern Ocean's response to abrupt climate change. This project aims to determine how the Southern Ocean responds to abrupt climate change, through geochemical analysis of marine sediment cores. Rapid warming events of the last ice age provide an analogue to human-caused warming. Experiments using ocean climate models will evaluate the drivers and consequences of the biogeochemical response of different sectors and zones of the Southern Ocean. The intended outcome is a better understanding of how and why climate change impacts ocean productivity in the ecologically significant Southern Ocean. This will lead to better representations of carbon feedbacks in climate models and more robust projections of future climate change.Read moreRead less
Are proposed land-based sinks for greenhouse gases resilient to climate change and natural variability? One strategy to reduce the scale of future climate change is to enhance the storage of carbon in vegetation and soils. Evidence suggests carbon stored in vegetation and soils is itself vulnerable to climate change, placing this stored carbon at risk; this project will assess this risk to advise on the reliability of using terrestrial systems as carbon sinks.
Australian Laureate Fellowships - Grant ID: FL150100090
Funder
Australian Research Council
Funding Amount
$2,770,434.00
Summary
Ocean mixing processes and innovation in oceanographic models. Ocean mixing processes and innovation in oceanographic models: This fellowship project aims to develop new oceanographic tools and thermodynamic variables to support a new generation of accurate ocean models more suitable for the prediction of changes in a warming world. The ocean’s role in the climate system is predominantly to store and to transport heat and carbon dioxide, and the ocean’s ability to do this is sensitive to the str ....Ocean mixing processes and innovation in oceanographic models. Ocean mixing processes and innovation in oceanographic models: This fellowship project aims to develop new oceanographic tools and thermodynamic variables to support a new generation of accurate ocean models more suitable for the prediction of changes in a warming world. The ocean’s role in the climate system is predominantly to store and to transport heat and carbon dioxide, and the ocean’s ability to do this is sensitive to the strength of mixing processes, which are quite uncertain. This project hopes to distinguish the vital role of vertical mixing from that of horizontal mixing by (i) developing algorithms to construct neutral density surfaces in climate models, (ii) formulating new inverse techniques to deduce the amount of vertical mixing in various ocean regions, and (iii) incorporating new approaches to ocean mixing processes and thermodynamics into ocean models.Read moreRead less
Are subterranean estuaries a source or sink of greenhouse gases? The aim of this project is to investigate the role of subterranean estuaries and submarine groundwater discharge on the marine cycle of the greenhouse gases carbon dioxide, methane, and nitrous oxide. The expected outcome of this project is a better understanding of the role of coastal environments as a net source or sink of greenhouse gases.