Researchers from the Department of Earth Sciences at the University of Oxford have shown that weathering of rocks in the Canadian Arctic will accelerate with rising temperatures, triggering a positive feedback loop that will release more and more CO2 to the atmosphere. The findings have been published in the journal Science Advances. Researchers from the Department of Earth Sciences at the University of Oxford have shown that weathering of rocks in the Canadian Arctic will accelerate with rising temperatures, triggering a positive feedback loop that will release more and more CO2 to the atmosphere. The findings have been published in the journal Science Advances. Earth Sciences Environment Phys.org – latest science and technology news stories