We may not think of heatwaves as big contributors to the nations mortality rate but research shows that extreme temperatures currently contribute to the deaths of over 1000 people aged over 65 each year across Australia (McMichael et al., 2003). They have been described as “silent killers”, causing more deaths since the 1890s than bushfires, cyclones, earthquakes, floods and severe storms combined. In fact, from 1844 to 2010, extreme heat events have been responsible for at least 5332 fatalities in Australia and, since 1900, 4555: more than the combined total of deaths from all other natural hazards. Over 30% of those deaths occurred in just nine events.

Deaths from Natural Hazards

What is a heatwave?

Before we look at the changing distribution of heatwave frequency and duration, it's best to define what the term means and how it is measured.

A heatwave is described by the Australian Bureau of Meteorology as three or more days of high maximum and minimum temperatures that are unusual for a given location (BOM, 2016). A heat wave always includes the combination of intensity and duration of high temperature periods.

Metrics used on the dashboard are:

Dashboard Metrics

What drives changes in heatwaves?

Heatwaves are primarily controlled by changes in temperature. Globally, for example, mean seasonal changes in temperature is responsible for 95% of projected heatwave changes in most regions (Argueso et al., 2016).

See the animation below for projected increases in annual temperature for Queensland

Fortunately, there seems to be good agreement about the nature of weather systems driving heatwaves in Australia. In many cases a high-pressure system sits next to the region experiencing the heatwave, pushing hot air from the centre of Australia towards that region. The location of the high depends on the region experiencing the heatwave, but there is always one there.

These high-pressure systems are created and sustained by other weather influences farther afield, for instance. We know for instance that heatwaves in Melbourne are coupled with tropical cyclones to the northwest of Australia.

Other, longer-term variables can affect not just individual heatwaves but their patterns, timing and severity too. So heatwaves are likely to be much longer and more frequent during El Niño than La Niña phases over much of northern and eastern Australia. However, this does not influence heatwaves over Australia’s far southeast – here, the most important driver is changes to wind patterns over the Southern Ocean.

Significantly more heatwave days, and longer and more intense events are observed over northern and eastern Australia during El Niño compared to La Niña (Perkins et al. 2015), yet different relationships occur in the southeast (Trewin 2009; Parker et al. 2014; Boschat et al. 2015).

But there is still a gap in our understanding of how future changes to patterns such as El Niño will influence our heatwaves.

Point and click to the figure elements to read original scientific publications about heatwave drivers.

Heat Waves

What does the model heat wave data say about the future for Queensland

The maps below show how heatwaves duration and frequency are projected to intensify across Queensland’s local government areas based on climate models simulations.

Point and click to a local government area in the map below and check the plots to understand how do climate models project future heatwaves across Queensland’s regions.

Plot values represented as anomalies (change in relation to reference period 1986-2005). Red line is multi-model average, grey shaded area indicates model spread or uncertainty and grey lines denote smoothed trends for average, minimum and maximum. Hover over the plots to change variable in the map.

Managing for the impacts of heatwaves

Heatwaves have direct impacts on mortality amongst the elderly and young but they also cause numerous indirect impacts such as stress on electricity networks, emergency services, hospitals and infrastructure stresses such as road damage and transport delays when railway lines buckled under the extreme conditions. The impacts of severe heatwaves are likely to affect all sectors of the Australian community, from the general public to government organizations and industries, health, utilities, commerce, agriculture and infrastructure. 

Impacts of Heat Waves in Australia

These impacts have led state governments and other bodies to investigate heatwave management strategies, while the Bureau of Meteorology have developed a heatwave forecast service for Australia. The Climate council have also summarized the extreme temperatures during the summer of 2016/2017.

In general, getting better prepared for the effects future heatwaves involves making progress in the following five principal adaptation areas:

Improve messaging and communication Consider heat in planning and development Define roles and responsibilities Improve existing building stock and infrastructure ITake account of heat in workplace health and safety

For example, in January 2018, the Queensland Government began the process of undertaking a detailed macro level risk assessment for heatwave. The project is a partnership between Queensland Fire and Emergency Services (QFES), Queensland Health and the Department of Environment and Science (DES). The key objectives of the assessment include:

  • Support Queensland Health in their role as the lead functional agency for heatwaves under the State Disaster Management Plan (SDMP);
  • Analyse and report on severe and extreme heatwave risk against the six exposed elements categories used in the Queensland Emergency Risk Management Framework (QERMF).

The project will be a collaborative effort across Governments and non-government organisations across the public and private sectors and involve substantial engagement at state and regional level. It will culminate in the publication of the State Heatwave Risk Assessment (planned for January 2019).

Some useful links in terms of public safety messaging and State level planning from the Queensland Government (incl. Q Health) are included below: