"Anthropogenic climate change is unfortunately a very significant risk to the long term continuation of human society on earth, as we know it."
Anthropology of Climate Change
The risk that carbon based climate change poses to modern society should not be overlooked.
Small changes in climate have played a role in the collapse of past societies. The collapse of the Nordic community on Greenland during the late 15th century has been attributed to a short term decrease in local temperatures of around 0.5 degrees Celsius (Diamond, 2005).
Over the next century, global temperatures may well reach over 4 degrees above pre-industrial. Global temperatures have not reached these levels since the middle of the Miocene epoch, around 14 million years ago.
Modern Climate Change History
A carbon based mechanism for climatic warming was proposed by Svante Arrhenius in 1896. Experimental evidence confirming a pattern of continually increasing atmospheric carbon dioxide levels was published in 1960, by C. Keeling.
By the late twentieth century the vast majority of the impartial scientific community had accepted the general principles of anthropogenic climate change. Today the broader community is very much aware of the link between atmospheric carbon and increasing global temperatures, and the potential for significant long term global average temperature increases.
Recent attempts at global co-operation to reduce the causes of anthropogenic climate change, such as commitments made at the Paris COP 21 UN Climate Summit, have produced strong rhetoric around capping global temperature increases to 2.0 degrees C above pre-industrial, with an aspirational goal of 1.5 degrees C. General scientific consensus is that the ecological and societal impacts of a global average temperature increase of between 1.5 and 2.0 degrees C will be create many challenges, but should still be managable.
Unfortunately emissions to date and continuing fossil fuel usage trends mean that we are on track for global average tempertures well above levels generally considered to be "manageable" in terms of impacts on natural and agricultural ecosystems.
Where is Our Climate Heading?
In 2016, global average temperatures reached 1.0 degree above the adopted 1870 baseline year for the first time, (UK Met Office, 2016). As the industrial revolution actually began in 1750, warming that occurred between 1750 and 1870 (0.2 degrees C) also needs to be accounted for, so average temperatures in 2016 were actually 1.2 degrees Celsius above a "genuine" pre-industrial baseline (Dunlop, 2016).
Some further temperature increases may already be "locked in", due to temperature increases lagging behind greenhouse gas emissions due to temperatue stabilisation from melting ice, ocean temperature stratification and a geological heat sink effect. Temperature lag may be significant, and could be as much as 0.6 degreees celcius (The Conversation, 2014).
A further temperature increase can also be expected when reflective sulphate pollutants from coal fire power stations that have a global cooling effect, are removed from our atmosphere, as these power stations are eventually phased out. This increase has been estimated to be as much as 0.5 degrees celcius, (Mann, 2015).
"Greenhouse gas emissions to date are expected to cause warming of more than 2.0 degrees Celsius above pre-industrial, even if greenhouse gas emissions were to end overnight. " (S. Brink, 2017)
So where to from here?
If greenhouse gas emissions continue in accordance Paris COP 21 commitments, (i.e. full fossil fuel use being phased out by 2100), temperatures can be expected to be around 4 degrees Celcius above pre-industrial by early next century.
"The consequences of a 4 degree celsius temperature increase above pre-industrial are immense. Widespread agro-economic, ecological and even human population collapses, are possible, and perhaps even likely? "