Tian, Hanqin; Xu, Rongting; Canadell, Josep G.; Thompson, Rona Louise; Winiwarter, Wilfried; Suntharalingam, Parvadha; Davidson, Eric A.; Ciais, Philippe; Jackson, Robert B.; Janssens-Maenhout, Greet; Prather, Michael J.; Regnier, Pierre; Pan, Naiqing; Pan, Shufen; Peters, Glen Philip; Shi, Hao; Tubiello, Francesco N.; Zaehle, Sönke; Zhou, Feng; Arneth, Almut; Battaglia, Gianna; Berthet, Sarah; Bopp, Laurent; Bouwman, Alexander F.; Buitenhuis, Erik T.; Chang, Jinfeng; Chipperfield, Martyn P.; Dangal, Shree R, S,; Dlugokencky, Edward; Elkins, James W.; Eyre, Bradley D.; Fu, Bojie; Hall, Bradley; Ito, Akihiko; Joos, Fortunat; Krummel, Paul B.; Landolfi, Angela; Laruelle, Goulven G.; Lauerwald, Ronny; Li, Wei; Lienert, Sebastian; Maavara, Taylor; Macleod, Michael; Millet, Dylan B.; Olin, Stefan; Patra, Prabir K.; Prinn, Ronald G.; Raymond, Peter A.; Ruiz, Daniel J.; van der Werf, Guido R.; Vuichard, Nicolas; Wang, Junjie; Weiss, Ray F.; Wells, Kelley C.; Wilson, Chris; Yang, Jia; Yao, Yuanzhi (Peer reviewed; Journal article, 2020)
Nitrous oxide (N2O), like carbon dioxide, is a long-lived greenhouse gas that accumulates in the atmosphere. Over the past 150 years, increasing atmospheric N2O concentrations have contributed to stratospheric ozone ...