BAMOS Vol 32 No.1 March 2019 | Page 27

BAMOS Mar 2019 Other key findings from the report: • Australia’s climate has warmed by just over 1 °C since 1910, leading to an increase in the frequency of extreme heat events (See Figure 1). • April to October rainfall has decreased in the southwest of Australia. Across the same region May–July rainfall has seen the largest decrease, by around 20 per cent since 1970. • There has been a decline of around 11 per cent in April– October rainfall in the southeast of Australia since the late 1990s. • Streamflow has decreased across southern Australia. Streamflow has increased in northern Australia where rainfall has increased. • There has been a long-term increase in extreme fire weather, and in the length of the fire season, across large parts of Australia. • Oceans around Australia have warmed by around 1 °C since 1910, contributing to longer and more frequent marine heatwaves. • The last two years (2016 and 2017) have seen mass bleaching over parts of the Great Barrier Reef in consecutive years for the first time, with the northern Reef experiencing bleaching in both summers. • Sea levels are rising around Australia, increasing the risk of inundation. • The world’s oceans are taking up more than 90 per cent of the extra energy stored by the planet as a result of enhanced greenhouse gas concentrations, and the southern hemisphere oceans have taken up the majority of this heat (Figure 2). • Australia is projected to experience: » » Further increases in sea and air temperatures, with more hot days and marine heatwaves, and fewer cool extremes. » » Further sea level rise and ocean acidification. » » Decreases in rainfall across southern Australia with more time in drought, but an increase in intense heavy rainfall throughout Australia. The Bureau of Meteorology and CSIRO play a key role in monitoring, measuring, understanding and reporting on weather and climate phenomena. State of the Climate draws on the best available peer-reviewed information including scientific observations based on multiple evidence sources. Watch the State of the Climate 2018 video. Read State of the Climate 2018. Figure 2. Estimated change in ocean heat content over the full ocean depth, from 1960 to 2017. Shading provides an indication of the confidence range of the estimate. Estimates of global ocean heat content have been enhanced in recent years with the deployment of thousands of robotic submersible floats worldwide, as part of the international Argo program. Note that data contributing to the early part of the record are sparse and trends estimated over this period are small compared to the error bars, hence considered unreliable. 27