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Investigations of the Diurnal Variation of Vertical HCHO Profiles Based on MAX-DOAS Measurements in Beijing: Comparisons with OMI Vertical Column Data

机译:基于MAX-DOAS的北京市垂直HCHO廓线日变化研究:与OMI垂直柱数据的比较

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An investigation into the diurnal characteristics of vertical formaldehyde (HCHO) profiles was conducted based on multi-axis differential optical absorption spectroscopy (MAX-DOAS) measurements in Beijing during the CAREBEIJING campaign, covering a month-long period through August and September 2006. Vertical HCHO profiles were retrieved based on a combined differential optical absorption spectroscopy (DOAS) technique and an optimal estimation method (OEM). The HCHO volume-mixing ratio (VMR) was found to be highest in the layer from the surface up to an altitude of 1 km and to decrease with altitude above this layer. In all retrieved profiles, HCHO was not detected in the layer from 3–4 km. Over the diurnal cycle, the HCHO VMR values were generally highest at 15:00 local time (LT) and were lower in the morning and late afternoon. The mean HCHO VMRs were 6.17, 1.82, and 0.80 ppbv for the 0–1, 1–2, and 2–3-km layers, respectively, at 15:00 LT, whereas they were 3.54 (4.79), 1.06 (1.43), and 0.46 (0.63) ppbv for the 0–1, 1–2, and 2–3-km layers, respectively, at 09:00 (17:00) LT. The HCHO VMRs reached their highest values at 15:00 LT on August 19, which were 17.71, 5.20, and 2.31 ppbv for the 0–1, 1–2, and 2–3-km layers, respectively. This diurnal pattern implies that the photo-oxidation of volatile organic compounds (VOCs) was most active at 15:00 LT for several days during the campaign period. In a comparison of the derived HCHO VCDs with those obtained from the Ozone Monitoring Instrument (OMI) measurements, the HCHO vertical column density (VCD) values obtained from the OMI measurements tend to be smaller than those from the MAX-DOAS.
机译:在CAREBEIJING活动期间,基于多轴差分光学吸收光谱(MAX-DOAS)测量,对北京的垂直甲醛(HCHO)日分布进行了调查,调查持续了一个月,直到2006年8月和2006年9月。基于组合的差分光学吸收光谱(DOAS)技术和最佳估计方法(OEM)检索HCHO轮廓。发现HCHO的体积混合比(VMR)在该层中从表面到1 km的高度最高,并随该层以上的高度降低。在所有检索到的剖面中,在3-4 km的层中均未检测到HCHO。在昼夜周期中,HCHO VMR值通常在当地时间15:00(LT)最高,而在早晨和下午较低。到15:00 LT,0-1、1-2和2-3-km层的平均HCHO VMR分别为6.17、1.82和0.80 ppbv,而它们分别为3.54(4.79),1.06(1.43) ,在LT的09:00(17:00),对于0、1、2和2–3公里的层分别为0.46(0.63)ppbv。 HCHO VMR在8月19日15:00 LT达到最高值,分别为0、1、2和2至3公里层分别为17.71、5.20和2.31 ppbv。这种昼夜模式表明,在运动期间,挥发性有机化合物(VOC)的光氧化在LT 15:00活跃了几天。在将导出的HCHO VCD与通过臭氧监测仪器(OMI)测量获得的VCD进行比较时,从OMI测量获得的HCHO垂直列密度(VCD)值往往小于从MAX-DOAS获得的HCHO VCD。

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