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Long-term tropospheric formaldehyde concentrations deduced from ground-based fourier transform solar infrared measurements

机译:从地面傅立叶变换太阳红外测量结果推导出的对流层甲醛长期浓度

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摘要

We report a 13-year (1992–2005) dataset of total column measurements offormaldehyde (HCHO) over Lauder, New Zealand, inferred from solar infraredspectra measured using a high-resolution Fourier Transform Spectrometer(FTS). Ambient HCHO concentrations at this rural location are often close tolevels typical of remote marine environments (250 ppt), which are closeto the detection limit using standard techniques. Consequently we develop anew method that successfully produces HCHO columns with sufficientsensitivity throughout the whole season. HCHO columns over Lauder have astrong seasonal cycle (±50%), with a mean column of 4.9×10 molecules cm,peaking during summer months. A simple box model ofCH oxidation reproduces the observed broad-scale seasonal cycle, butsignificantly underestimates the seasonal peak HCHO ground concentrationsduring summer. This suggests the existence of an additional significantsource of HCHO, possibly isoprene that cannot be explained by oxidation ofCH alone. The ground-based FTS column data compare well withcollocated HCHO column measurements from the Global Ozone MonitoringExperiment (GOME) satellite instrument during the operational period of GOME(1996–2001, =0.65, mean bias=10%, =48).
机译:我们报告了使用高分辨率傅里叶变换光谱仪(FTS)测得的太阳红外光谱推断出的13年(1992–2005年)新西兰劳德市甲醛(HCHO)总色谱柱数据集。在这个农村地区,环境HCHO的浓度通常接近偏远海洋环境的典型水平(<250 ppt),接近标准技术的检测极限。因此,我们开发了一种新方法,可以在整个季节内成功生产出具有足够灵敏度的HCHO色谱柱。 Lauder上的HCHO色谱柱具有较强的季节性周期(±50%),平均色谱柱为4.9×10分子cm cm,在夏季月份达到峰值。一个简单的CH氧化盒模型可以再现观察到的广泛的季节性周期,但是大大低估了夏季夏季HCHO地面浓度的季节性峰值。这表明存在HCHO的其他重要来源,可能是异戊二烯,不能单独用CH氧化来解释。在GOME的运行期间(1996-2001,= 0.65,平均偏差= 10%,= 48),地面FTS柱数据与全球臭氧监测实验(GOME)卫星仪器的并置HCHO柱测量结果很好。

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