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HOsubx/sub observations over West Africa during AMMA: impact of isoprene and NOsubx/sub

机译:AMMA期间西非的HO x 观测:异戊二烯和NO x 的影响

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Aircraft OH and HO2 measurements made over West Africa during the AMMA fieldcampaign in summer 2006 have been investigated using a box model constrained to observationsof long-lived species and physical parameters. "Good" agreement was found forHO2 (modelled to observed gradient of 1.23 ± 0.11). However, the modelsignificantly overpredicts OH concentrations. The reasons for this are not clear, but mayreflect instrumental instabilities affecting the OH measurements. Within themodel, HOx concentrations in West Africa are controlled by relatively simplephotochemistry, with production dominated by ozone photolysis and reaction of O(1D)with water vapour, and loss processes dominated by HO2 + HO2 andHO2 + RO2. Isoprene chemistry was found to influence forestedregions. In contrast to several recent field studies in very low NOx and highisoprene environments, we do not observe any dependence of model success for HO2 onisoprene and attribute this to efficient recycling of HOx through RO2 + NOreactions under the moderate NOx concentrations (5–300 ppt NO in the boundary layer, median 76 ppt)encountered during AMMA. This suggests that some of the problems with understandingthe impact of isoprene on atmospheric composition may be limited to the extreme low range ofNOx concentrations.
机译:使用限制于观察长寿物种和物理参数的盒模型,研究了2006年夏季在AMMA野外运动期间在西非进行的飞机OH和HO 2 测量。发现HO 2 具有“良好”的一致性(建模为观察到的1.23±0.11的梯度)。但是,该模型明显高估了OH浓度。其原因尚不清楚,但可能反映出影响OH测量的仪器不稳定。在该模型中,西非的HO x 浓度是通过相对简单的光化学控制的,其生产主要由臭氧光解和O( 1 D)与水蒸气的反应以及损失过程决定。由HO 2 + HO 2 和HO 2 + RO 2 主导。发现异戊二烯化学影响林区。与最近在非常低的NO x 和高异戊二烯环境中进行的几项现场研究相比,我们没有观察到HO 2 异戊二烯模型成功的任何依赖关系,而是将其归因于有效的H在中等NO x 浓度(边界层NO为5-300 ppt,中位数为76 ppt)下发生HO x 至RO 2 + NO反应在AMMA期间。这表明了解异戊二烯对大气成分影响的一些问题可能仅限于NO x 浓度的极低范围。

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