High biogenic volatile organic compound emissions but NOx-constrained ozone formation over a tropical island: A case study of Hainan Island, China

IF 3.4 Q2 ENVIRONMENTAL SCIENCES
Atmospheric Environment: X Pub Date : 2026-04-01 Epub Date: 2026-05-21 DOI:10.1016/j.aeaoa.2026.100467
Rongfu Xie , Xiaochen Wu , Chunmei Peng , Wenshuai Xu , Xinxin Meng , Daocheng Gong , Yuzhen Fu , Xiaocong Cao , Zhaohui Yang , Aidan Xian , Ruipeng Wang , Zike Qiu , Yating Song , Qiao Xing , Boguang Wang
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引用次数: 0

Abstract

Biogenic volatile organic compounds (BVOCs) are important precursors of tropospheric ozone (O3), yet their emissions and photochemical effects remain poorly characterized in tropical island regions of China. Using the Model of Emissions of Gases and Aerosols from Nature (MEGAN), driven by satellite-based land cover, Moderate Resolution Imaging Spectroradiometer (MODIS) vegetation products, and Weather Research and Forecasting (WRF) meteorology, we developed a high-resolution BVOC emission inventory for Hainan Island in 2019. The WRF model coupled with the Comprehensive Air Quality Model with Extensions (WRF-CAMx) was further applied to quantify summertime BVOC contributions to ozone formation through emission sensitivity simulations and photochemical regime diagnostics. Total BVOC emissions were estimated at 5.51 × 105 tons (t), with an annual mean emission intensity of 16.02 tons per square kilometer per year (t·km−2·yr−1), indicating strong biogenic emission potential under tropical conditions. Emissions peaked in summer (42.1%) and were lowest in winter (8.5%), but showed a weaker seasonal contrast than many continental regions of China, reflecting persistent evergreen vegetation activity and relatively small seasonal variations in temperature and radiation. Although BVOCs dominated the regional volatile organic compound (VOC) budget, their contribution to surface ozone was moderate. In July 2019, BVOCs increased regional mean ozone by 1.2 parts per billion (ppb), accounting for 3.67% of total ozone, with localized enhancements mainly in northern and northeastern Hainan. Empirical Kinetic Modeling Approach (EKMA) and relative incremental reactivity (RIR) analyses showed that ozone formation was predominantly nitrogen oxides (NOx)-limited across most of the island, with transitional NOx–VOC co-control in northern urbanized areas. These results reveal a high-BVOC but NOx-constrained photochemical environment, where abundant biogenic emissions do not necessarily cause strong island-wide ozone enhancement because ozone production is limited by NOx availability and modulated by regional transport. This study provides a baseline assessment of BVOC emissions and ozone impacts in tropical island ecosystems and suggests that ozone mitigation in Hainan should prioritize anthropogenic NOx reduction, with coordinated NOx–VOC control in northern urbanized areas.
热带岛屿上高生物源性挥发性有机化合物排放与nox约束的臭氧形成:以海南岛为例
生物源性挥发性有机化合物(BVOCs)是对流层臭氧(O3)的重要前体,但其在中国热带岛屿地区的排放和光化学效应特征尚不明确。利用自然气体和气溶胶排放模型(MEGAN),在卫星土地覆盖、中分辨率成像光谱仪(MODIS)植被产品和天气研究与预报(WRF)气象的驱动下,开发了2019年海南岛高分辨率BVOC排放清单。WRF模型与综合空气质量模型扩展(WRF- camx)结合,通过排放敏感性模拟和光化学状态诊断,进一步量化夏季BVOC对臭氧形成的贡献。BVOC总排放量估计为5.51 × 105吨(t),年平均排放强度为16.02吨/平方公里/年(t·km−2·yr−1),表明热带条件下具有很强的生物源排放潜力。排放量在夏季达到峰值(42.1%),在冬季最低(8.5%),但与中国许多大陆区域相比,季节性差异较弱,反映出常绿植被活动持续,温度和辐射的季节性变化相对较小。虽然BVOCs主导区域挥发性有机化合物(VOC)预算,但其对地表臭氧的贡献是中等的。2019年7月,BVOCs使区域平均臭氧增加1.2 十亿分之一(ppb),占臭氧总量的3.67%,局部增强主要在海南北部和东北部。经验动力学建模方法(EKMA)和相对增量反应性(RIR)分析表明,岛上大部分地区的臭氧形成主要受氮氧化物(NOx)限制,北部城市化地区则过渡性地受NOx和voc的共同控制。这些结果揭示了一个高bvoc但受NOx限制的光化学环境,其中大量的生物源排放并不一定会引起全岛范围内的强烈臭氧增强,因为臭氧产生受到NOx可用性的限制并受区域运输的调节。本研究提供了热带岛屿生态系统BVOC排放和臭氧影响的基线评估,并建议海南的臭氧缓解应优先考虑人为减少NOx,并协调北方城市化地区的NOx - voc控制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Atmospheric Environment: X
Atmospheric Environment: X Environmental Science-Environmental Science (all)
CiteScore
8.00
自引率
0.00%
发文量
47
审稿时长
12 weeks
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