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Seasonality of the lower tropospheric ozone over China observed by the Ozone Monitoring Instrument

机译:臭氧监测仪观测到的中国对流层低层臭氧的季节性

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摘要

We analyzed the ozone (O-3) profile product (PROFOZ) derived from Ozone Monitoring Instrument(OMI) ultraviolet (UV) spectra to reveal spatial and temporal variations in O-3 distributions over China. Although discriminating vertical O-3 in the lower troposphere is a challenge for satellite-borne measurements, previous research has confirmed the reliability of the lowermost layer O-3 of the PROFOZ product, corresponding to 0-3 km, under the high O-3 condition over China by comparison with the airborne measurements. In the present study, we focus on the seasonal variation of O-3 obtained in the lowermost layer over China. We track the O-3 enhancement under polluted conditions by using the ozone anomaly (Delta O-3), defined as the difference between the retrieval values and a priori values, because our focus is the temporally high O-3 level compared with the background level. We divide the 25-40 degrees N and 100-135 degrees E region into clusters according to the similarity of the seasonal variation in Delta O-3 at the lowermost layer corresponding to approximately 0-3 km in altitude. Using this cluster analysis, we distinguish the areas in which Delta O-3 has outstanding seasonality with high values in summer, particularly in June, and low values in winter over the North China Plain and Sichuan basin. The areas with these anomalous Delta O-3 values correspond to high NO2 emission areas. We compare the results with model simulations from the Meteorological Research Institute-Chemistry Climate Model (MRI-CCM2) and meteorological data. The areas showing outstanding seasonality also correspond to those of high chemical production rates in June. Along the coastal area, Delta O-3 values tend to drop to negative in August, which can be attributed to the inflow of clean oceanic air to inland regions. The results presented here again demonstrate the reliability of the lower tropospheric O-3 data from the OMI PROFOZ product and suggest good capability of UV satellite sensors for monitoring O-3 pollution that will be launched in the near future.
机译:我们分析了源自臭氧监测仪器(OMI)紫外线(UV)光谱的臭氧(O-3)剖面产物(PROFOZ),以揭示中国O-3分布的时空变化。尽管分辨低层对流层的垂直O-3对卫星测量是一个挑战,但先前的研究已确认PROFOZ产品最底层O-3的可靠性(在高O-3的情况下,对应于0-3 km)与空中测量结果相比,中国的状况。在本研究中,我们重点研究在中国最下层获得的O-3的季节变化。我们通过使用臭氧异常(Delta O-3)来跟踪在污染条件下的O-3增强,臭氧异常是指取回值与先验值之间的差,因为我们的关注点是与背景相比在时间上处于较高的O-3水平水平。我们根据最底层0-3 km处最底层的O-3三角洲季节变化的相似性,将25-40度N和100-135度E区域分为几类。使用这种聚类分析,我们可以分辨出华北平原和四川盆地的三角洲O-3具有突出的季节特征,夏季特别是六月,夏季值很高,冬季特别低。这些具有Delta O-3异常值的区域对应于高NO2排放区域。我们将结果与气象研究所-化学气候模型(MRI-CCM2)的模型模拟和气象数据进行了比较。季节性表现突出的地区也与6月份化学品的高生产率地区相对应。沿海地区,三角洲O-3值在8月份趋于下降,这可以归因于清洁的海洋空气流入内陆地区。此处提供的结果再次证明了OMI PROFOZ产品的对流层O-3较低数据的可靠性,并暗示了将在不久的将来启动的紫外线卫星传感器监测O-3污染的良好能力。

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