Multimetric analysis uncovers time-dependent climate forcings from China’s 2.3-fold cropland reactive nitrogen emissions

P Peng Xu Z Zhenzhong Zeng H Huizhong Shen (School of Environmental Science and Engineering, Southern University of Science and Technology) M Min Hu M Mingxu Liu (China-Australia Joint Research Center for Functional Molecular Materials, College of Materials Science and Engineering) C Cheng Gong Y Yilin Chen (School of Urban Planning and Design, Peking University, Shenzhen Graduate School) C Chaopu Ti (State Key Laboratory of Soil and Sustainable Agriculture, Changshu National Agro-Ecosystem Observation and Research Station, Institute of Soil Science, Chinese Academy of Sciences) G Geng Li (Department of Chemistry, State Key Laboratory of Marine Pollution, City University of Hong Kong, Hong Kong 999077, P. R. China) X Xuejing Wang (Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University) Y Yi Zheng S Si-Liang Li (Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University) C Cong-Qiang Liu (Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University) B Benjamin Z. Houlton (Department of Ecology and Evolutionary Biology, Cornell University)

Abstract

China is the largest emitter of cropland gaseous reactive nitrogen (Ngr, including NH 3 , N 2 O, and NOx), which greatly affects regional air quality, climate change, and human health. Despite the substantial spatial and temporal variations in cropland Ngr emissions, their driving mechanisms and net climate change forcings (either cooling or warming) remain unclear. Using revised emission estimates and bottom–up mass flow-based approaches, we evaluated the spatiotemporal changes in and key drivers of China’s cropland Ngr emissions from 1978 to 2023. We assessed the relative contribution of China’s cropland Ngr emissions to climate change via multiple metrics (global warming and temperature potentials). China’s cropland Ngr emissions increased by approximately 2.3-fold from 1978 to 2023. The pace of this increase decelerated over time, from 0.17 Tg N·y −2 before 1996 to 0.15 Tg N·y −2 during 1997–2005 and −0.05 Tg N·y −2 after 2005. Population growth and N-intensive animal-sourced food production accounted for 31.7% and 23.2% of this historical emission change, respectively. The net climate change forcing of Ngr varies with scale. Currently, China’s cropland Ngr emissions in 2017 at the county level impart a net cooling effect ascribed to short-lived NH 3 and NOx emissions, but this forcing shifts in sign and magnitude to a warming effect over a one-hundred-year time horizon, primarily through long-lived N 2 O emissions. Our findings suggest that a combination of metrics can comprehensively and adequately capture short-, medium-, and long-term climate impacts and that achieving climate targets will conspire against Ngr mitigation efforts for environmental protection goals.

Article Details

Volume / Issue Vol. 123, Issue 15
Published April 14, 2026
ISSN 0027-8424
Publisher National Academy of Sciences

Authors (14)

P

Peng Xu

Z

Zhenzhong Zeng

H

Huizhong Shen

School of Environmental Science and Engineering, Southern University of Science and Technology

M

Min Hu

M

Mingxu Liu

China-Australia Joint Research Center for Functional Molecular Materials, College of Materials Science and Engineering

C

Cheng Gong

Y

Yilin Chen

School of Urban Planning and Design, Peking University, Shenzhen Graduate School

C

Chaopu Ti

State Key Laboratory of Soil and Sustainable Agriculture, Changshu National Agro-Ecosystem Observation and Research Station, Institute of Soil Science, Chinese Academy of Sciences

G

Geng Li

Department of Chemistry, State Key Laboratory of Marine Pollution, City University of Hong Kong, Hong Kong 999077, P. R. China

X

Xuejing Wang

Institute of Ecology, College of Urban and Environmental Sciences and Key Laboratory for Earth Surface Processes of Ministry of Education, Peking University

Y

Yi Zheng

S

Si-Liang Li

Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University

C

Cong-Qiang Liu

Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University

B

Benjamin Z. Houlton

Department of Ecology and Evolutionary Biology, Cornell University