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作 者:程巳阳 马建中 周怀刚[2] 靳军莉[3] 刘岩[4] 董璠 周礼岩 颜鹏[1,3] CHENG Si-yang;MA Jian-zhong;ZHOU Huai-gang;JIN Jun-li;LIU Yan;DONG Fan;ZHOU Li-yan;YAN Peng(State Key Laboratory of Severe Weather&Key Laboratory of Atmospheric Chemistry of China Meteorological Administration,Chinese Academy of Meteorological Sciences,Beijing 100081 ,China;Shangdianzi Regional Air Background Station,Beijing Meteorological Bureau, Beijing 101507,China;China Meteorological Administration Meteorological Observation Center,Beijing 100081,China;College of Geographic Science and Tourism,Xinjiang Normal University,Urumqi 830054,China)
机构地区:[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
出 处:《光谱学与光谱分析》2018年第11期3470-3475,共6页Spectroscopy and Spectral Analysis
基 金: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NO_2 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NO_2 柱浓度反演研究。在NO_2 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NO_2 对流层垂直柱浓度(VCD_(trop))。观测期间NO_2 VCD_(trop)平均值和最大值分别为5.43×10^(15)和7.15×10^(16) molec·cm^(-2)。NO_2 VCD_(trop)日均值浓度水平较低,但总体上有上升趋势。NO_2 VCD_(trop)变化过程与风速风向关系密切:西南风时风速越小NO_2 VCD_(trop)越低,东北风对NO_2 VCD_(trop)有扩散稀释作用。NO_2 VCD_(trop)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NO_2 VCD_(trop)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。NO_2 VCD_(trop)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NO_2 VCD_(trop),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。In order to explore the variation characteristics of significant air pollutant N O 2 in the Beijing-Tianjin-Hebei background region,the Multi Axis Different ial Optical Absorption Spectroscopy(MAX-DOAS)was used to record solar scatter ing spectra at Shangdianzi regional atmospheric background station and retrieve the NO 2 column densities.Quantitative spectral analysis was carried out in t he characteristic wavelength of NO 2 405~430 nm.The NO 2 tropospheric verti cal column densities(VCD trop)from July 2009 to September 2009 were calc ulated through geometric approximation.The mean and maximum value of NO 2 VCD tr op were 5.43×10 15 and 7.15×10 16 molec·cm-2 during the observation period,respectively.The daily NO 2 VCD trop was lower,bu t there was an upward trend as a whole.The variation of NO 2 VCD trop wa s closely related to wind speed and direction:NO 2 VCD trop concentratio n was lower when southwesterly wind was weaker,and the northeasterly wind was conducive to the NO 2 diffusion.Generally,diurnal variations of NO 2 VC D trop showed the characteristics of being low at noon and high in the mo rning and evening,and the evening peak was slightly higher than the morning on e.The level and diurnal range of NO 2 VCD trop at Shangdianzi station we re significantly smaller than the results in the Beijing city over the same peri od.These variation characteristics were consistent with the ones at the mild p ollution stations of Xianghe and Gucheng in Hebei.In a word,reginal backgroun d atmospheric NO 2 VCD trop can be effectively monitored by MAX-DOAS,al though the characteristics were related to complex factors such as industrial an d traffic emission,photochemical reaction and atmospheric transport.More data a re necessary for further study.
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
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