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Climate change can accelerate due to feedback mechanisms: complex phenomena caused by climate change which in turn can further boost climate change. One example of this is the additional CO2 emission from thawing permafrost. Research into the long-term influence of feedback mechanisms has already been going on for a long time, just like research into modern climate change, of course, but the connection between both has so far been underexposed.

Jorien vonkWouter petersUtrecht university gert jan reichartDutch research councilRoyal netherlands institute for sea researchCaroline slomp radboud university nijmegenUtrecht universityProfessor of paleoceanography at utrecht universityResearch centreInstitute for marineWageningen university researchRadboud university nijmegenBack researchRoyal netherlands instituteSea researchWageningen university