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Satellite evidence for a large source of formic acid from boreal and tropical forests

机译:卫星证据表明来自北方和热带森林的大量甲酸

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Formic acid contributes significantly to acid rain in remote environments. Direct sources of formic acid include human activities, biomass burning and plant leaves. Aside from these direct sources, sunlight-induced oxidation of non-methane hydrocarbons (largely of biogenic origin) is probably the largest source. However, model simulations substantially underpredict atmospheric formic acid levels, indicating that not all sources have been included in the models. Here, we use satellite measurements of formic acid concentrations to constrain model simulations of the global formic acid budget. According to our simulations, 100- 120Tg of formic acid is produced annually, which is two to three times more than that estimated from known sources. We show that 90% of the formic acid produced is biogenic in origin, and largely sourced from tropical and boreal forests. We suggest that terpenoids- volatile organic compounds released by plants- are the predominant precursors. Model comparisons with independent observations of formic acid strengthen our conclusions, and provide indirect validation for the satellite measurements. Finally, we show that the larger formic acid emissions have a substantial impact on rainwater acidity, especially over boreal forests in the summer, where formic acid reduces pH by 0.25- 0.5.
机译:甲酸对偏远环境中的酸雨有很大贡献。甲酸的直接来源包括人类活动,生物量燃烧和植物叶片。除了这些直接来源外,阳光诱导的非甲烷碳氢化合物(主要是生物起源)的氧化可能是最大的来源。但是,模型模拟大大低估了大气中甲酸的含量,这表明并非所有来源都已包含在模型中。在这里,我们使用甲酸浓度的卫星测量值来约束全球甲酸预算的模型模拟。根据我们的模拟,每年生产100-120Tg甲酸,这是从已知来源估计的产量的两到三倍。我们表明,所产生的90%的甲酸是生物成因的,并且大部分来自热带和北方森林。我们建议萜类化合物(植物释放的挥发性有机化合物)是主要的前体。与甲酸的独立观测值进行模型比较可加强我们的结论,并为卫星测量提供间接验证。最后,我们表明,较大的甲酸排放量对雨水的酸度有重大影响,特别是在夏季的北方森林中,甲酸会使pH值降低0.25-0.5。

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