GC018-08
Agricultural Fertilization Drives Increased Seasonal Amplitude of CO2 Exchange

Monday, 7 December 2020: 17:58
Virtual
Danica Lombardozzi1, William R Wieder2, Gretchen Keppel-Aleks3, David M Lawrence1, Xin Lin4, Gordon B Bonan1, Charles Koven5, Pierre Friedlingstein6 and Keith T Lindsay7, (1)National Center for Atmospheric Research, Boulder, CO, United States, (2)National Center for Atmospheric Research, Climate and Global Dynamics Laboratory, Boulder, CO, United States, (3)University of Michigan Ann Arbor, Climate and Space Sciences and Engineering, Ann Arbor, MI, United States, (4)LSCE Laboratoire des Sciences du Climat et de l'Environnement, Gif-Sur-Yvette, France, (5)Lawrence Berkeley National Laboratory, Berkeley, CA, United States, (6)University of Exeter, Exeter, United Kingdom, (7)NCAR, Boulder, CO, United States
Abstract:
The terrestrial carbon sink is growing with anthropogenic emissions and increasing the amplitude of the annual CO2 cycle by up to 50% in northern latitudes over the past 50 years. While previous work highlights the important role of increasing CO2 concentrations and warmer temperatures, many studies cannot fully explain the factors contributing to the increased amplitude. Here, we use CESM2, which simulates CO2 amplitude at Barrow more accurately than older model versions, to explore the extent to which CO2 concentrations, climate change, land use change, agricultural N fertilization and irrigation contribute to changes in the annual CO2 cycle in the Northern Hemisphere. Our analysis highlights that industrial nitrogen (N) fertilization has a disproportionately large influence on the increasing CO2 amplitude in northern latitudes, increasing the CO2 amplitude in the northern hemisphere during 1995-2015 by 3 ppm on average and up to 9 ppm in some regions. Higher CO2 concentrations and warmer temperatures also increase the amplitude of carbon fluxes, although the overall impact is smaller. Land use change and irrigation are locally important, but have negligible large-scale impacts. These results illustrate the importance of agricultural N fertilization in regulating annual carbon cycle fluxes and highlight that ESMs can improve the seasonal CO2 cycle by representing agricultural N fertilization.