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Surface and boundary layer exchanges of volatile organic compounds, nitrogen oxides and ozone during the GABRIEL campaign

机译:GABRIEL活动期间挥发性有机化合物,氮氧化物和臭氧的表面和边界层交换

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We present an evaluation of sources, sinks and turbulent transport ofnitrogen oxides, ozone and volatile organic compounds (VOC) in the boundarylayer over French Guyana and Suriname during the October 2005 GABRIELcampaign by simulating observations with a single-column chemistry andclimate model (SCM) along a zonal transect. Simulated concentrations ofO3 and NO as well as NO2 photolysis rates over the forest agreewell with observations when a small soil-biogenic NO emission flux wasapplied. This suggests that the photochemical conditions observed duringGABRIEL reflect a pristine tropical low-NOx regime. The SCM uses acompensation point approach to simulate nocturnal deposition and daytimeemissions of acetone and methanol and produces daytime boundary layer mixingratios in reasonable agreement with observations. The area average isopreneemission flux, inferred from the observed isoprene mixing ratios andboundary layer height, is about half the flux simulated with commonlyapplied emission algorithms. The SCM nevertheless simulates too highisoprene mixing ratios, whereas hydroxyl concentrations are stronglyunderestimated compared to observations, which can at least partly explainthe discrepancy. Furthermore, the model substantially overestimates theisoprene oxidation products methlyl vinyl ketone (MVK) and methacrolein(MACR) partly due to a simulated nocturnal increase due to isopreneoxidation. This increase is most prominent in the residual layer whereas inthe nocturnal inversion layer we simulate a decrease in MVK and MACR mixingratios, assuming efficient removal of MVK and MACR. Entrainment of residuallayer air masses, which are enhanced in MVK and MACR and other isopreneoxidation products, into the growing boundary layer poses an additional sinkfor OH which is thus not available for isoprene oxidation. Based on thesefindings, we suggest pursuing measurements of the tropical residual layerchemistry with a focus on the nocturnal depletion of isoprene and itsoxidation products.
机译:我们通过模拟单柱化学和气候模型(SCM)的观测资料,对2005年10月GABRIELcampaign上法属圭亚那和苏里南边界层的氮氧化物,臭氧和挥发性有机化合物(VOC)的源,汇和湍流传输进行了评估。地带样带。森林中模拟的O 3 和NO以及NO 2 的光解浓度与土壤生物源NO排放通量较小时的观测结果吻合。这表明GABRIEL期间观察到的光化学条件反映了原始的热带低NO x 方案。 SCM使用补偿点方法模拟丙酮和甲醇的夜间沉积和白天排放,并产生与观测值合理吻合的白天边界层混合比。由观察到的异戊二烯混合比和边界层高度推断出的面积平均异戊二烯通量大约是常用排放算法模拟的通量的一半。然而,SCM模拟的异戊二烯混合比例太高,而与观察值相比,羟基浓度被大大低估了,这至少可以部分解释这一差异。此外,该模型实质上高估了异戊二烯的氧化产物甲基甲苯基乙烯基酮(MVK)和甲基丙烯醛(MACR)的部分原因是由于异戊二烯氧化导致的夜间睡眠增加。假设有效去除了MVK和MACR,则这种增加在残留层中最为明显,而在夜间反转层中,我们模拟了MVK和MACR混合比的降低。在MVK和MACR和其他异戊二烯氧化产物中增强的残留层空气质量被夹带到生长的边界层中,这造成了额外的OH吸收,因此不可用于异戊二烯氧化。基于这些发现,我们建议对热带残留层化学进行测量,重点是夜间消耗异戊二烯及其氧化产物。

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