Changing Weather – Northern Cassowary Coast

Ave max temp variation Innisfail

Figure 1. Variation (°C) from the long-term (1969-2019) average (orange line) in annual average maximum temperatures in the Northern Cassowary Coast region (BOM data from Innisfail). The shape of the blue line in the graph shows the natural, observed variation in average temperatures between years – we all know that some years are hotter than others. By comparing the blue line to the orange line, we can see how this variation relates to the long-term average of temperature; above the orange line, average annual maximum temperatures are hotter than the long term average, whereas below the orange line they are cooler than average.

Rainfall variation Northern Cassowary Coast

Figure 2. Variation (mm) from the long-term (1969-2019) average (yellow line) in annual rainfall totals in the Northern Cassowary Coast region (BOM data from South Johnstone Experimental Station).

Ave max temp increase NT - multiple years

Figure 3. Projected increase in average maximum temperatures from the observed historical average temperatures from Innisfail (1970-2015, blue line) to 2030 (yellow line, based on climate model Had GEM2-ES), 2070 (orange line, model GISS-E2-R-CC), and 2090 (red line, model IPSL-CM5B-L2).


Number of days over 35°C in Innisfail

Current 2030 2050 2070 2090
2 2 9 15 30

Figure 4. Number of days over 35°C under ‘Business as usual’ emissions scenario (MIROC5 climate model)

Sea level rise in Cairns

Year 2030 2090
Height (m) 0.14 0.65

Figure 5. Increased height needed to maintain the current level of exposure of assets to flooding from high tides & storm surges, under ‘Business as usual’ emissions scenario,

Changing weather in more locations

To access changing weather data from other locations in the Wet Tropics, click on the links in the table below.

Daintree Changing WeatherDouglas Changing WeatherCairns Region Changing Weather
Russell & Mulgrave Catchments Changing WeatherNorthern Tablelands Changing WeatherSouthern Tablelands Changing Weather
Northern Cassowary Coast Changing WeatherSouthern Cassowary Coast Changing WeatherUpper Herbert Changing Weather
Hinchinbrook Changing Weather

We are already witnessing changes in weather observations in our Local Landscape, in particular a rising trend in temperatures. People on the Northern Cassowary Coast know that our ability to live in and manage the landscape is based on long experience of general seasonal patterns, but many will say that knowledge based on past experience is becoming less reliable. This will have a range of implications for people living in our Local Landscape, and the science is already telling us:

  • Less predictable weather: Ongoing climate change will make it increasingly difficult to rely on our past experience to make decisions about where to build houses and infrastructure, which crops to grow, which pests and diseases to target, and how to protect native species.
  • Climate change and industries: Put very simply, temperatures will increase and it will stay hotter for longer, while the risk of extreme weather events will increase.  These factors will result in challenges to our landscape’s major industries, like sugar cane, bananas, fishing and tourism, however there may also emerge new agricultural and commercial opportunities.
  • Climate change and communities: While climate change will affect everyone in some way, being informed about the types of changes likely to occur in our local landscape will allow us to plan and prepare, rather than being taken by surprise by unusual climate events.
  • Climate change and natural systems: Our natural systems have always been exposed to changes, however the rate of change occurring in recent times with regard to climate conditions means some species or ecosystems may not be able to keep up or adapt in time.

There will be opportunities for everyone to get involved in shaping a resilient and sustainable future for the Northern Cassowary Coast.  For more information on climate change, including links to more detailed climate change modelling for our region, go to the Climate Futures page.

Less predictable weather

Long-term temperature records from Innisfail show that average temperatures have generally been on an increasing trend over the past 20 years, and that during this time, average annual temperatures in the region have been above the long-term average much more often than they have been below it (Figure 1).

Long-term rainfall data from the South Johnstone experimental station show that total rainfall continues to vary dramatically between years, and that there is no obvious increasing or decreasing trend in annual rainfall at this stage (refer to Figure 2).

As time goes on, higher temperatures will be reached more frequently. For example, maximum daily temperatures during January are projected to increase from the current average of 30.8°C to 32.3°C by 2030, 32.4°C by 2070 and 33.7°C by 2090 (Figure 3). Furthermore, there will be a longer season of high temperatures, with the average daily maximum temperature exceeding 30°C from October to April by 2090.

While we are likely to see an increasing trend in temperatures as a result of climate change, one of the most concerning predictions coming from climate scientists is the impact of greater variability and less predictability in our weather patterns, making it harder to plan.

Climate change and industries

Sugar cane and banana production will be directly affected by increasing average temperatures, evaporation, heat waves, extreme rainfall events and increasing atmospheric carbon dioxide. For example, the sucrose content of sugarcane can decline if temperatures are high and/or there is high rainfall during the ripening and harvest season ( Similarly, the growth and development of bananas is reduced by temperatures outside the optimum range of 25-30°C (, and north Queensland growers may lose their advantage if winters warm sufficiently in southern growing locations to enable an all-year growing season. Areas of cultivation in low-lying coastal areas will obviously also be vulnerable to sea level rise and growers have bitter experience of the damage that can be caused by tropical cyclones. Climate change may also bring new diseases and pests, which we know potentially pose enormous threats to our agricultural industries. Flooding associated with extreme rainfall will also affect waterways and floodplains, potentially increasing erosion in these areas.

Regional primary industries may also be impacted by increasing bottlenecks in processing or distribution networks. For example, heat waves, cyclones and floods all have the potential to result in shut down of industrial operations such as the Tully and South Johnstone sugar mills, either through workplace health and safety concerns, power failure, flooding or damage. Operation of facilities such as the Cairns and Mourilyan sea ports will also be affected by storm surge, cyclones, flooding during heavy rainfall, and extreme heat. Considering the importance of ports to both the import of fuel, food and other supplies, as well as to the export of regional produce, more frequent closures are likely to have significant economic implications for the region.

Climate change will also impact the commercial fishing industry. For example, intense cyclones can cause several months of lost operations due to large amounts of debris or sediment in the water and damage to boats, marinas, ramps and other infrastructure. Commercial fishing operations will be affected as certain types of fish move south due to increasing water temperatures, as coral bleaching becomes more widespread and as conditions decline in fish breeding and nursery areas.

Tourism in the area is underpinned by the natural values of the coast and mainland forest areas. Climate-induced changes in the health and composition of natural systems, including the potential loss of iconic species (see below), will potentially have major impacts on tourism in the area. Since tourism is already very seasonal, prolonged hot weather and less predictable rainfall is likely to affect visitation patterns, while more extreme weather may influence tourists’ perception of their safety in the region.

Changing climatic conditions will challenge our established ways of doing things, but may also present new agricultural and commercial opportunities. For example, it may be necessary to diversify or switch crops or breeds to suit new climatic conditions, or to change practices. In order to adapt to new and changing climatic conditions, we may need to shift farming and other commercial enterprises to different parts of the landscape. This could create opportunities for the restoration of wildlife habitat on former agricultural land, but could also create conflict between the need to protect existing habitat and also maintain production.

 Climate change and communities

Doing things the way they’ve been done for generations won’t necessarily keep working as climate conditions continue to change, meaning that traditions and local wisdom will be challenged. Everyone will be affected in one way or another by climate change: some types of farms may not remain viable, certain areas along the coastline may become unsafe to live, and some of our iconic species may not survive in the new conditions. While change can be unsettling, new opportunities may come out of new ways of doing things, especially by working together across sectors and industries. Importantly, being informed about the types of changes we can reasonably expect means that we can develop plans and strategies to adapt to these, rather than being taken by surprise by unusual climate events.

Although people along the Northern Cassowary Coast are used to living with high temperatures, we can expect that periods of extreme heat will become more common and even hotter. For example, the number of days hotter than 35°C in Innisfail is projected to increase from the current average of two to nine by 2050 under the ‘business as usual’ emissions scenario (Figure 4). More people will be vulnerable to heat-related illnesses and stress, especially sick, elderly and very young people, and people living without air-conditioning.

In the same way that maximum temperatures are increasing (Figure 3), minimum temperatures are also rising. This means that overnight temperatures will remain above 20°C for more months of the year, potentially affecting sleep quality, especially for households without air conditioning, and increasing the use of air conditioning in households with it.

Sea levels are already rising and models project that sea levels in this region will increase by an average of 0.14 m by the year 2030, and by an average of 0.65 m by 2090 under a business as usual emissions scenario. By 2030, homes and other assets along the Northern Cassowary coastline would need to be 0.14 m higher (0.79 m in 2090) to maintain their current level of exposure to flooding from the ocean (Figure 5). Low elevation areas of the coastline will be most vulnerable.

Rising sea levels will increase the tidal extent of coastal rivers and streams, meaning that the tidal reach in the North and South Johnstone Rivers may push further upstream, potentially affecting homes, businesses and crops on adjacent floodplains, as well as roads and other infrastructure. Even a modest increase in sea level height will mean that there are many more high tides and storm surges, increasing coastal erosion, flooding and contaminating freshwater systems with salt water.  The CoastAdapt tool ( helps people making decisions in coastal areas to understand and asses the risks posed by climate change in their regions.

The impacts of sea level rise will be compounded by more frequent and intense heavy rainfall events in the region, as well as more intense (though probably less frequent) tropical cyclones. There will be an increased threat to homes, businesses and roads to the extensive low-lying areas along the Northern Cassowary coastline from river flooding and storm surge and cyclonic winds. People living in buildings that can’t withstand severe cyclones will be very vulnerable during cyclonic winds. Local planning for development, stormwater drains, roads and bridges will be affected. We can expect more frequent interruptions to grid-based electricity supply as well as to fuel and other supplies due to shut down of the region’s rail lines, sea and air ports during extreme weather events. Working together to address back-up power and supply issues will help build the Northern Cassowary Coast’s resilience in the face of these changes. 

Various programs are available to assist with developing and implementing adaptation strategies (for example, the QCoast2100 program for local governments to develop Coastal Hazard Adaptation Strategies

Climate change and natural systems

Natural systems have coped with changing climatic conditions in the past but current changes are happening so fast that some species may not be able to adapt. Because climatic factors such as temperature and rainfall play such an important role in determining the suitability of different areas for plants and animals, we can expect that changes in temperature and rainfall will change the suitability of the landscape for certain species and systems. The result of climate change will be new combinations of plants and animals, sometimes in new locations, challenging our concept of what is ‘natural’. It’s also likely that this region will become more attractive to people moving from other areas that become less liveable. Increasing pressure for housing and more infrastructure to support growing populations will potentially lead a push for more clearing of native vegetation.

The Northern Cassowary Coast is likely to retain climate conditions that suit many of the species that are currently found here. However, some animals and plants may no longer be able to survive or reproduce in the area. For example, habitat for cassowaries will be impacted by sea level rise, with the loss of coastal freshwater wetlands, and by changes in the fruiting patterns of plants resulting from warmer temperatures and changed rainfall. Modelling shows ( that areas along the region’s coastline are likely to rapidly become less suitable for cassowaries as temperatures increase over the next decade. Under a business as usual scenario of greenhouse gas emissions, suitable climatic conditions will continue to decline and will be lost from the coastal plain by the year 2085. In these models, suitable climate for cassowaries will contract to the foothills and ranges at higher altitudes in the west of the region. This modelling also shows that climatic conditions on the eastern slopes of the range may become suitable for the mahogany glider, even though this species doesn’t currently inhabit these areas. In reality, changes may not unfold exactly as these models project, but these projections have complex implications for how we manage landscapes to protect our plants and animals; we have to protect areas that are currently important so that threatened species survive, but also consider where important habitat will likely be in the future, together with whether and how plants and animals would be able to move there and establish. These considerations affect our decisions about which areas to protect and restore, as well as how to manage factors such as fire in these areas.

Coastal species in particular are at risk from sea level rise, for example:

  • Critically endangered littoral rainforest systems are under extreme threat from climate change, as beaches are inundated and freshwater wetlands and coastal scrub transition to salt-tolerant vegetation communities. These natural systems protect a diversity of threatened plants and animals, as well as protecting coastal settlements.
  • There will be fewer nesting beaches for sea turtles.
  • A range of birds and mammals will be affected by the loss of freshwater wetlands as beaches and dune systems are inundated or eroded.
  • Freshwater wetlands and coastal floodplains, together with the abundant wildlife they support, are also under threat from more intense flooding during heavy rainfall events and salt water contamination due to sea level rise and storm surge.
  • We can expect widespread dieback of sea grasses and mangroves in lower intertidal zones, due to sea level rise, more intense cyclones and storm surges, affecting fish, dugong and other estuarine and marine life.

Strategies such as the planned retreat of human settlements and infrastructure from coastal areas may reduce the risk to humans and also create opportunities for natural systems to shift landward.

In addition to the direct effects of increased temperatures and changed rainfall, climate change will have a range of indirect effects on other factors that drive natural systems. A major impact of climate change for natural systems will be more frequent and/or more intense disturbances, such as floods, heatwaves and cyclones. For example, increased intensity and frequency of river flooding, together with increased water temperatures, will change aquatic systems, as well as those fringing waterways or on floodplains. Narrow riparian vegetation will be particularly vulnerable. More extreme rainfall events will also increase the frequency of intense disturbance to in-stream invertebrates, animals and plants, and exacerbate the issue of soil and pollutant runoff entering the region’s wetlands and the Great Barrier Reef lagoon. On a national scale, the North and South Johnstone Rivers are among a small number of watercourses identified as being priorities for conservation of freshwater biodiversity under climate change.

Prospects are bleak for the Great Barrier Reef under a business as usual scenario of climate change. Bleaching of coral reefs will continue to be more widespread as average temperatures increase and heatwaves become hotter and more common. As hot spells occur more frequently, reefs won’t have time to recover from previous bleaching episodes and will eventually collapse. Reef systems will also be affected by more acidic sea water (caused by higher CO2), more intense cyclones and freshwater pulses associated with heavy rainfall events.

Managers of biodiversity are already working to minimise or reverse impacts of land clearing, pollution, introduced plants, animals and diseases on natural systems. Climate change is an additional impact that interacts with these existing pressures. The resilience of natural systems to cyclones and other disturbances is improved by having a large and well-managed network of protected areas. It’s not possible to predict the exact consequences of climate change for plants, animals and their habitats, but sharing observations, trying new management practices and monitoring their outcomes will help build the new knowledge required to promote adaptation of natural systems to climate change.