Selected intervals in the past that were as warm or warmer than today can help us understand what the Earth may be like under future global warming.
A latest assessment of past warm periods, published today in Nature Geoscience by an international team of 59 scientists from 17 nations, shows that in response to the warming ecosystems and climate zones will spatially shift and on millennial time scales ice sheets will substantially shrink.
Selected intervals in the past that were as warm or warmer than today can help us understand what the Earth may be like under future global warming.
A latest assessment of past warm periods, published today in Nature Geoscience by an international team of 59 scientists from 17 nations, shows that in response to the warming ecosystems and climate zones will spatially shift and on millennial time scales ice sheets will substantially shrink.
The study was an outcome of a workshop that took place in Bern, Switzerland and was coordinated by the University of Bern, the University of New South Wales in Australia, and Oregon State University.
The compiled evidence from the past suggests that even with a global warming limited to within 2 degrees Celsius above preindustrial levels, as aimed at in the Paris Agreement, climate zones and ecosystems will shift, rapid polar warming may release additional greenhouse gases, and sea-level will rise by several meters over several thousand years. These observations show that many current climate models designed to project changes within this century may underestimate longer-term changes.
Over the past 3.5 million years, several time intervals are known for being .5 to 2 degrees Celsius warmer than the so-called preindustrial temperatures of the 19th century. These intervals reveal much stronger regional warming at high latitudes than in the tropics, similar to what models predict for a 2 degrees Celsius global warming by the year 2100. Although not all these past warmings were caused by higher carbon dioxide concentrations, they are helpful to assess the regional effect of a warming of a scale comparable to that aimed at in the Paris Agreement.
Read more at Oregon State University
Graph Credit: NASA / JPL-Caltech
