Okrah Abraham, Magara Genesis, Mensah Caleb, Yeboah Emmanuel, Prempeh Nana Agyemang, Yawlui Ignatius Senyo Yao, Nyasulu Mathews, Asante Vincent Antwi, Junior Innocent John, Sarfo Isaac
School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, 210044, China.
Department of Atmospheric and Climate Science, School of Geosciences, University of Energy and Natural Resources, Sunyani, Ghana.
Environ Monit Assess. 2025 Jul 8;197(8):876. doi: 10.1007/s10661-025-14361-3.
East Africa (EA) faces significant challenges related to greenhouse gas (GHG) emissions, particularly carbon dioxide (CO₂) and methane (CH₄), largely driven by biomass burning (BB) from agricultural fires and wildfires. Despite their importance, the spatiotemporal variability of these emissions remains poorly understood. This study quantifies CO₂ and CH₄ emissions across EA (2001-2022), revealing significant CO₂ emission peaks in 2005 (32.5 million tonnes), 2016 (29.8 million tonnes), and 2020 (31.2 million tonnes), alongside an 18% increase in CH₄ emissions between 2015 and 2020. BB accounted for approximately 54% of total CO₂ emissions (17 million tonnes) and 74% of CH₄ emissions (16 million tonnes), with regional hotspots including Northern Uganda (NUG), Tanzania (TZ), and South Sudan (SS) exhibiting the highest intensities, especially during dry seasons where emissions surged by up to 40%. Analysis of regional trends reveals a significant decline in CO₂ emissions in the Western Transition (WTZ) (slope = -13.02, p = 0.0004), likely reflecting effective mitigation such as forest restoration and REDD+ programs, supported by satellite-observed greening. In contrast, SS, NUG, and the Southeastern Tanzania (SETZ) showed negative but statistically insignificant CO₂ trends, indicative of fluctuating land-use pressures rather than sustained mitigation. CH₄ emissions rose significantly in the WTZ (slope = 15.67, p = 0.0001), driven by agricultural intensification, with a marginal increase in NUG, while remaining stable in SS and the SETZ. Non-stationarity in emissions (ADF p > 0.05) across regions highlights the influence of dynamic socio-environmental factors such as land-use changes, policy shifts, and climate variability. These findings emphasize the urgent need for improved fire management, sustainable land practices, and integrated mitigation strategies to address EA's growing environmental threats and contribute to global climate goals under the Paris Agreement.
东非(EA)面临与温室气体(GHG)排放相关的重大挑战,特别是二氧化碳(CO₂)和甲烷(CH₄),主要由农业火灾和野火的生物质燃烧(BB)驱动。尽管这些排放很重要,但其时空变化仍知之甚少。本研究量化了2001 - 2022年整个东非的CO₂和CH₄排放,揭示了2005年(3250万吨)、2016年(2980万吨)和2020年(3120万吨)出现显著的CO₂排放峰值,同时2015年至2020年期间CH₄排放增加了18%。生物质燃烧占总CO₂排放(约1700万吨)的约54%和CH₄排放(约1600万吨)的74%,区域热点包括乌干达北部(NUG)、坦桑尼亚(TZ)和南苏丹(SS),其强度最高,特别是在旱季,排放量激增高达40%。区域趋势分析显示,西部过渡区(WTZ)的CO₂排放显著下降(斜率 = -13.02,p = 0.0004),这可能反映了有效的缓解措施,如森林恢复和REDD+计划,并得到卫星观测到的绿化的支持。相比之下,南苏丹、乌干达北部和坦桑尼亚东南部(SETZ)的CO₂趋势呈负但统计上不显著,表明土地利用压力波动而非持续缓解。西部过渡区的CH₄排放显著上升(斜率 = 15.67,p = 0.0001),由农业集约化驱动,乌干达北部略有增加,而在南苏丹和坦桑尼亚东南部保持稳定。各区域排放的非平稳性(ADF p > 0.05)突出了土地利用变化、政策转变和气候变率等动态社会环境因素的影响。这些发现强调迫切需要改进火灾管理、可持续土地实践和综合缓解战略,以应对东非日益增长的环境威胁,并为《巴黎协定》下的全球气候目标做出贡献。