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上甸子区域大气本底站NO2柱浓度光谱反演及其变化特征
作者单位:1. 灾害天气国家重点实验室和中国气象局大气化学重点开放实验室,中国气象科学研究院,北京 100081
2. 北京市气象局上甸子区域大气本底站,北京 101507
3. 中国气象局气象探测中心,北京 100081
4. 新疆师范大学地理科学与旅游学院,新疆 乌鲁木齐 830054
基金项目:国家自然科学基金项目(41505123,41075095),中国气象科学研究院基本科研业务费专项(2015Y002)资助
摘    要:为了探究京津冀本底浓度地区NO2这一重要空气污染物的变化特征,采用多轴差分吸收光谱技术(MAX-DOAS)在上甸子区域大气本底站开展了太阳散射光谱观测以及NO2柱浓度反演研究。在NO2的405~430nm特征谱段进行了定量光谱解析,并通过几何近似法计算了2009年7~9月NO2对流层垂直柱浓度(VCDtrop)。观测期间NO2 VCDtrop平均值和最大值分别为5.43×1015和7.15×1016 molec·cm-2。NO2 VCDtrop日均值浓度水平较低,但总体上有上升趋势。NO2 VCDtrop变化过程与风速风向关系密切:西南风时风速越小NO2 VCDtrop越低,东北风对NO2 VCDtrop有扩散稀释作用。NO2 VCDtrop日变化形态总体上呈现为中午时段低、早晚较高的特征,并且傍晚峰值比早间峰值略高。上甸子站NO2 VCDtrop浓度水平和日变化幅度相比北京城区同期观测结果明显偏小。NO2 VCDtrop变化特征与河北香河和固城等污染相对较轻站点观测到的变化特征相一致。总之,MAX-DOAS能够有效监测区域本底大气的NO2 VCDtrop,其变化特征与工业和交通排放、大气光化学过程、大气传输等复杂因素有关,还需积累更多数据和深入研究。

关 键 词:多轴差分吸收光谱技术  二氧化氮  柱浓度  区域大气本底站  
收稿时间:2017-11-01

Spectral Inversion and Characteristics of NO2 Column Density at Shangdianzi Regional Atmospheric Background Station
Authors:CHENG Si-yang  MA Jian-zhong  ZHOU Huai-gang  JIN Jun-li  LIU Yan  DONG Fan  ZHOU Li-yan  YAN Peng
Institution:1. State Key Laboratory of Severe Weather & Key Laboratory of Atmospheric Chemistry of China Meteorological Administration, Chinese Academy of Meteorological Sciences, Beijing 100081, China 2. Shangdianzi Regional Air Background Station, Beijing Meteorological Bureau, Beijing 101507, China 3. China Meteorological Administration Meteorological Observation Center, Beijing 100081, China 4. College of Geographic Science and Tourism,Xinjiang Normal University,Urumqi 830054,China
Abstract:In order to explore the variation characteristics of significant air pollutant NO2 in the Beijing-Tianjin-Hebei background region, the Multi Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) was used to record solar scattering spectra at Shangdianzi regional atmospheric background station and retrieve the NO2 column densities. Quantitative spectral analysis was carried out in the characteristic wavelength of NO2 405~430 nm. The NO2 tropospheric vertical column densities (VCDtrop) from July 2009 to September 2009 were calculated through geometric approximation. The mean and maximum value of NO2 VCDtrop were 5.43×1015 and 7.15×1016 molec·cm-2 during the observation period, respectively. The daily NO2 VCDtrop was lower, but there was an upward trend as a whole. The variation of NO2 VCDtrop was closely related to wind speed and direction: NO2 VCDtrop concentration was lower when southwesterly wind was weaker, and the northeasterly wind was conducive to the NO2 diffusion. Generally, diurnal variations of NO2 VCDtrop showed the characteristics of being low at noon and high in the morning and evening, and the evening peak was slightly higher than the morning one. The level and diurnal range of NO2 VCDtrop at Shangdianzi station were significantly smaller than the results in the Beijing city over the same period. These variation characteristics were consistent with the ones at the mild pollution stations of Xianghe and Gucheng in Hebei. In a word, reginal background atmospheric NO2 VCDtrop can be effectively monitored by MAX-DOAS, although the characteristics were related to complex factors such as industrial and traffic emission, photochemical reaction and atmospheric transport. More data are necessary for further study.
Keywords:MAX-DOAS  NO2  Column density  Regional atmospheric background station  
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