2.5°C

Predicted Global Warming

Without dramatic emissions reductions, global average temperatures could be 2.5°C higher than pre-industrial levels by 2050.

<iframe title="Predicted Global Temperature Increases" aria-label="Interactive line chart" id="datawrapper-chart-btt3O" src="//datawrapper.dwcdn.net/btt3O/4/" scrolling="no" frameborder="0" style="width: 0; min-width: 100% !important; border: none;" height="380"></iframe><script type="text/javascript">!function(){"use strict";window.addEventListener("message",function(a){if(void 0!==a.data["datawrapper-height"])for(var e in a.data["datawrapper-height"]){var t=document.getElementById("datawrapper-chart-"+e)||document.querySelector("iframe[src*='"+e+"']");t&&(t.style.height=a.data["datawrapper-height"][e]+"px")}})}();
</script>

The graph above shows the predicted global temperature increases for four different scenarios of future greenhouse gas levels. The greater the temperature increase the greater the risks to ecosystems and human society. A temperature increase greater than 1.5°C is considered dangerous, and greater than 3.0°C is likely to be catastrophic. Under all the scenarios global temperature increases are likely to reach dangerous levels before 2040.

The data for the graph was derived from the outputs of CMIP5 (Coupled Model Intercomparison Project phase 5) climate models – an ensemble of coupled ocean-atmosphere general circulation models (GCMs), which were used in producing the IPCC Fifth Assessment Report.

Climate models are mathematical simulations of the Earth’s climate system. The models utilise scenarios for future greenhouse gas emissions to generate predictions of future climate change. The scenarios which form the inputs to the models are called Representative Concentration Pathways (RCPs). The RCPs consist of detailed sets of figures for potential future emissions of greenhouse gases, and their resulting atmospheric concentrations, which provide a common baseline for running climate models. Each RCP defines an emissions trajectory which results in a particular level of radiative forcing in 2100.

Data

The data for this graph was downloaded from the KNMI Climate Change Atlas. The settings used are shown in the following image:

References

1. ‘KNMI Climate Explorer: Climate Change Atlas, GCM: CMIP5 (IPCC AR5 Atlas Subset)’ (KNMI – Royal Netherlands Meteorological Institute) http://climexp.knmi.nl/plot_atlas_form.py?id=someone@somewhere [accessed 8 January 2020] [↩]