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Deep Adaptation


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Part I The Predicament

       Jem Bendell and Rupert Read

      Climate science was probably born in 1896 with the first, and still valid, calculation of how much the earth would warm if atmospheric CO2 content were to double from pre-industrial values (Arrhenius 2009 [1896]). Given the means of the day, without the use of electronic computers, the Swedish physicist Svante Arrhenius, famous for his contributions to thermodynamics and the understanding of chemical reactions, calculated that the earth would warm by about 4°C. His value still lies within the range of modern estimates, produced by hugely complicated computer models (Slingo 2017). Arrhenius even calculated that regions near the poles would warm much more than those near the equator, something that is still seen as a major finding of climate science.

      Awareness of humanity’s vulnerability to changes in climate was high at the close of the nineteenth century. Arrhenius’s native Scandinavia and much of northern Europe had only recently come out of the Little Ice Age, a cold period that had led to frequent crop failure and starvation (Lee 2009). His hope was therefore that increasing amounts of ‘carbonic acid’ in the air – atmospheric carbon dioxide – would bring about better weather and increased crop yields for the colder regions of the earth.

      Human interest in understanding the geological past has created a different branch of climate science a long time ago, now called paleo-climatology. On its own, paleo-climatology can already tell us a compelling story of where we are and further help us understand the scale of our calamity. By drilling deep holes into Antarctic ice and analysing the composition of tiny bubbles found in them, researchers have been able to construct a continuous record of atmospheric carbon dioxide going back