PROJECT 5.3: Regional climate change projections science and delivery To make informed decisions about managing current and future climate risks, decision-makers across government, industry and business require access to credible,…
Project 2.6
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In this webinar John Clarke provided a demonstration of the Thresholds Calculator tool within the Climate Change in Australia website to estimate the frequency of future hot, cold, wet and dry extremes under different emissions scenarios.
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20 December 2018 Michael Grose and Lynette Bettio Michael Grose is the Lead Chief Investigator in the ESCC Hub’s Project 2.6: Regional climate projections science, information and services, which is…
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Hub researchers are continuing to develop our understanding of the processes driving southern Australia’s rainfall, including the causes of our declining winter rainfall, the seasonality of rainfall, and the occurrence of extreme rainfall in southern Australia.
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In this webinar, Dr Michael Grose talks about climate change projections research undertaken by the Earth System and Climate Change Hub, how climate projections have been produced in the past and where they could go in the future.
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Hub researchers are investigating the processes that influence rainfall in northern Australia, so we can better understand how they are changing and what this means for the timing and amount of rainfall.
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In this webinar, Dr Josephine Brown talks about her work with climate models looking at rainfall changes in northern Australia.
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In this webinar John Clarke provides a demonstration of how to use the Climate Analogues tool and tailor the results to meet individual needs. A brief introduction to the Climate Change in Australia website is also provided.
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Managing climate risk to 2030 means accounting for both climate change and natural climate variability.
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Climate projections from the early 1990s are showing themselves to be in line with observations, but natural climate variability influences our perception of reliability.
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Climate projections provide important information to help make decisions about the future, but projecting what the climate is likely to look like in 10 or 100 years is a little different to predicting tomorrow’s weather.