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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得出的长期对流层甲醛浓度

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摘要

We report a 13-year (1992-2005) dataset of total column measurements of formaldehyde (HCHO) over Lauder, New Zealand, inferred from solar infrared spectra measured using a high-resolution Fourier Transform Spectrometer (FTS). Ambient HCHO concentrations at this rural location are often close to levels typical of remote marine environments (<250 ppt), which are close to the detection limit using standard techniques. Consequently we develop a new method that successfully produces HCHO columns with sufficient sensitivity throughout the whole season. HCHO columns over Lauder have a strong seasonal cycle (±50%), with a mean column of 4.9×10~(15) molecules cm ~(-2), peaking during summer months. A simple box model of CH _4 oxidation reproduces the observed broad-scale seasonal cycle, but significantly underestimates the seasonal peak HCHO ground concentrations during summer. This suggests the existence of an additional significant source of HCHO, possibly isoprene that cannot be explained by oxidation of CH_4 alone. The ground-based FTS column data compare well with collocated HCHO column measurements from the Global Ozone Monitoring Experiment (GOME) satellite instrument during the operational period of GOME (1996-2001, r~2=0.65, mean bias=10%, n=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在新西兰劳德市的甲醛(HCHO)总甲醛测量值的13年(1992-2005)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〜(15)分子cm〜(-2),在夏季月份达到峰值。 CH _4氧化的简单盒模型可重现观察到的大规模季节性周期,但大大低估了夏季的季节性峰值HCHO地面浓度。这表明存在HCHO的其他重要来源,可能是异戊二烯,不能通过单独CH_4的氧化来解释。在GOME的运行期间(1996-2001,r〜2 = 0.65,平均偏差= 10%,n = 48)。

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