Autor/es reacciones

Pep Canadell

Executive Director of the Global Carbon Project and Senior Research Fellow at the CSIRO Climate Science Centre in Canberra, Australia

This study demonstrates the high level of planetary disruption due to climate change, now with a possible new global warming feedback mechanism that few studies have previously shown to be of great importance: a growth in methane emissions due to increased precipitation in marshy areas of the tropics and higher temperatures in cold boreal areas, including those with permafrost.  

What we don't need now is the discovery of new planetary feedback mechanisms that could accelerate global warming. 

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