Global mapping of crop-specific emission factors highlights hotspots of nitrous oxide mitigation

环境科学 土壤学 全球变暖 减缓气候变化 环境资源管理 大气科学 气候变化 土壤科学 土壤水分 生态学 生物 地质学
作者
Xiaoqing Cui,Feng Zhou,Philippe Ciais,Eric A. Davidson,Francesco N. Tubiello,Xiaoyue Niu,Xiaotang Ju,Josep G. Canadell,Lex Bouwman,Robert B. Jackson,Nathaniel D. Mueller,Xunhua Zheng,David Kanter,Hanqin Tian,Wulahati Adalibieke,Yan Bo,Qihui Wang,Xiaoying Zhan,Dongqiang Zhu
出处
期刊:Nature food [Springer Nature]
卷期号:2 (11): 886-893 被引量:177
标识
DOI:10.1038/s43016-021-00384-9
摘要

Mitigating soil nitrous oxide (N2O) emissions is essential for staying below a 2 °C warming threshold. However, accurate assessments of mitigation potential are limited by uncertainty and variability in direct emission factors (EFs). To assess where and why EFs differ, we created high-resolution maps of crop-specific EFs based on 1,507 georeferenced field observations. Here, using a data-driven approach, we show that EFs vary by two orders of magnitude over space. At global and regional scales, such variation is primarily driven by climatic and edaphic factors rather than the well-recognized management practices. Combining spatially explicit EFs with N surplus information, we conclude that global mitigation potential without compromising crop production is 30% (95% confidence interval, 17–53%) of direct soil emissions of N2O, equivalent to the entire direct soil emissions of China and the United States combined. Two-thirds (65%) of the mitigation potential could be achieved on one-fifth of the global harvested area, mainly located in humid subtropical climates and across gleysols and acrisols. These findings highlight the value of a targeted policy approach on global hotspots that could deliver large N2O mitigation as well as environmental and food co-benefits. Estimating the global cropland N2O mitigation potential is limited by the uncertainty and variability of direct emission factors (EFs). Here, using a data-driven approach with 1,507 chamber-based field observations of EFs, the study shows that EF variation is primarily driven by climatic and edaphic factors. Two-thirds of the mitigation potential could be achieved on one-fifth of the global harvested area, mainly located in humid subtropical climates and across gleysols and acrisols.
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