Three decades of global methane sources and sinks

  title={Three decades of global methane sources and sinks},
  author={Stefanie Kirschke and Philippe Bousquet and Philippe Ciais and Marielle Saunois and Josep G. Canadell and Edward J. Dlugokencky and Peter Bergamaschi and Daniel Bergmann and Donald R. Blake and Lori Bruhwiler and Philip J. Cameron-Smith and Simona Castaldi and Fr{\'e}d{\'e}ric Chevallier and Lianghuan Feng and Annemarie Fraser and Martin Heimann and Elke L. Hodson and Sander Houweling and B{\'e}atrice Josse and Paul J. Fraser and Paul B. Krummel and Jean‐François Lamarque and Ray L. Langenfelds and Corinne Le Qu{\'e}r{\'e} and Vaishali Naik and Simon J. O'Doherty and Paul I. Palmer and Isabelle Pison and David A. Plummer and Benjamin Poulter and Ronald G. Prinn and Matthew L. Rigby and Bruno Ringeval and Monia Santini and Martina Schmidt and Drew T. Shindell and Isobel Simpson and Renato Spahni and L. Paul Steele and Sarah A. Strode and Kengo Sudo and Sophie Szopa and Guido van der Werf and Apostolos Voulgarakis and Michiel van Weele and Ray F. Weiss and J. E. Ffowcs Williams and Guang Zeng},
  journal={Nature Geoscience},
Methane is an important greenhouse gas, responsible for about 20% of the warming induced by long-lived greenhouse gases since pre-industrial times. By reacting with hydroxyl radicals, methane reduces the oxidizing capacity of the atmosphere and generates ozone in the troposphere. Although most sources and sinks of methane have been identified, their relative contributions to atmospheric methane levels are highly uncertain. As such, the factors responsible for the observed stabilization of… Expand

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