Lin, X., Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI 48109, United States; Rogers, B.M., Woods Hole Research Center, Falmouth, MA 02540, United States; Sweeney, C., Global Monitoring Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO 80305, United States; Chevallier, F., Laboratoire des Sciences du Climat et de l’Environnement, Institut Pierre Simon Laplace, Commissariat à l’Énergie Atomique et aux Énergies Alternatives–CNRS, Université de Versailles Saint-Quentin-en-Yvelines, Université Paris-Saclay, Gif-sur-Yvette, F-91191, France; Arshinov, M., Vladimir Evseevich Zuev Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences, Tomsk, 634055, Russian Federation; Dlugokencky, E., Global Monitoring Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO 80305, United States; Machida, T., Center for Global Environmental Research, National Institute for Environmental Studies, Tsukuba, Ibaraki 305-8506, Japan; Sasakawa, M., Center for Global Environmental Research, National Institute for Environmental Studies, Tsukuba, Ibaraki 305-8506, Japan; Tans, P., Global Monitoring Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO 80305, United States; Keppel-Aleks, G., Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI 48109, United States
Recommended Citation:
Lin X.,Rogers B.M.,Sweeney C.,et al. Siberian and temperate ecosystems shape Northern Hemisphere atmospheric CO2 seasonal amplification[J]. Proceedings of the National Academy of Sciences of the United States of America,2020-01-01,117(35)