Climate Change in Australia
Climate information, projections, tools and data
Recently, there have been times when the world has been more than 1.5 °C warmer than the average pre-industrial temperature – individual months and even a 12-month period at (July 2023 to June 2024). However, we have not yet reached the 1.5 °C global warming level. This is because reaching a warming level is based on a longer-term average, not a single month or year. The 20-year moving average of the global mean surface air temperature (GSAT) needs to be at or very near +1.5 °C relative to the pre-industrial climate. At that time, the +1.5 °C warming level will have been reached, and this is what we are calling a “+1.5 °C world”. The same conditions are used to define +2, +3 and +4 °C global warming levels.
We are projected to be at the 1.5 °C global warming level in around 2030 under all plausible scenarios of global change. We would stabilise the global average temperature at 1.5 °C only under extremely ambitious emissions reductions.
The date at which the world will first reach a particular global warming level is determined by three factors:
The possibility of reaching of +2, +3 and +4 °C levels, and the timing of reaching them are very strongly affected by the emissions pathway (see graphs below).
The amount of warming for a given increase in greenhouse gas concentration (known as climate sensitivity) is not precisely known, so this creates a range of possible dates a warming level is reached for a given emissions pathway.
Climate variability not only affects when a warming level will be temporarily reached, such as the 12-month period over 1.5 °C we have recently experienced but processes of longer-term variability such as the Inter-decadal Pacific Oscillation (IPO) could also affect when the longer-term average reaches the warming level, by 5 years or more.
In reality, there is little chance that the world would plateau precisely at any particular warming level permanently. But even if it did, the regional climate would not instantly be at a new steady state.
Because the climate system has considerable inertia, some things take a while to reach a new steady state, or new ‘equilibrium’. Slower processes like sea level rise take hundreds of years to fully reach a new equilibrium, so the sea level will be lower in the first years of a +1.5 °C world compared to if the climate has stabilised at +1.5 °C for a long period. But global warming levels are a useful benchmark to assess climate change this century.
The IPCC Sixth Assessment Report produced estimated windows of reaching global warming levels, assessed from observations, various climate models, and our understanding of climate sensitivity. Here are these windows represented visually for two commonly used SSPs, showing the time period where reaching the level is possible (lines) and the central estimate if it is present (circles):
Page last updated 19th May 2025