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首页> 外文期刊>Atmospheric Measurement Techniques Discussions >Evaluating Sentinel-5P TROPOMI tropospheric NO2 column densities with airborne and Pandora spectrometers near New York City and Long Island Sound
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Evaluating Sentinel-5P TROPOMI tropospheric NO2 column densities with airborne and Pandora spectrometers near New York City and Long Island Sound

机译:在纽约市和长岛声音附近,评估Sentinel-5P Tropomi TroperiC No2柱密度和长岛声音的空中和潘多拉光谱仪

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摘要

Airborne and ground-based Pandora spectrometer NO2 column measurements were collected during the 2018 Long Island Sound Tropospheric Ozone Study (LISTOS) in the New York City/Long Island Sound region, which coincided with early observations from the Sentinel-5P TROPOspheric Monitoring Instrument (TROPOMI) instrument. Both airborne- and ground-based measurements are used to evaluate the TROPOMI NO2 Tropospheric Vertical Column (TrVC) product v1.2 in this region, which has high spatial and temporal heterogeneity in NO2. First, airborne and Pandora TrVCs are compared to evaluate the uncertainty of the airborne TrVC and establish the spatial representativeness of the Pandora observations. The 171 coincidences between Pandora and airborne TrVCs are found to be highly correlated (r2=0.92 and slope of 1.03), with the largest individual differences being associated with high temporal and/or spatial variability. These reference measurements (Pandora and airborne) are complementary with respect to temporal coverage and spatial representativity. Pandora spectrometers can provide continuous long-term measurements but may lack areal representativity when operated in direct-sun mode. Airborne spectrometers are typically only deployed for short periods of time, but their observations are more spatially representative of the satellite measurements with the added capability of retrieving at subpixel resolutions of 250m×250m over the entire TROPOMI pixels they overfly. Thus, airborne data are more correlated with TROPOMI measurements (r2=0.96) than Pandora measurements are with TROPOMI (r2=0.84). The largest outliers between TROPOMI and the reference measurements appear to stem from too spatially coarse a priori surface reflectivity (0.5°) over bright urban scenes. In this work, this results during cloud-free scenes that, at times, are affected by errors in the TROPOMI cloud pressure retrieval impacting the calculation of tropospheric air mass factors. This factor causes a high bias in TROPOMI TrVCs of 4%–11%. Excluding these cloud-impacted points, TROPOMI has an overall low bias of 19%–33% during the LISTOS timeframe of June–September?2018. Part of this low bias is caused by coarse a priori profile input from the TM5-MP model; replacing these profiles with those from a 12km North American Model–Community Multiscale Air Quality (NAMCMAQ) analysis results in a 12%–14% increase in the TrVCs. Even with this improvement, the TROPOMI-NAMCMAQ TrVCs have a 7%–19% low bias, indicating needed improvement in a priori assumptions in the air mass factor calculation. Future work should explore additional impacts of a priori inputs to further assess the remaining low biases in TROPOMI using these datasets.
机译:在纽约市/长岛声音地区的2018年长岛声音对流层臭氧研究(Listos)期间收集了空中和地面的潘多拉光谱仪No2柱测量,这与Sentinel-5P对流层监测仪(Tropomi的早期观测相吻合) 仪器。空中和地基测量均用于评估该区域的Tropomi No2对流层垂直柱(TRVC)产品V1.2,其在NO 2中具有高空间和时间异质性。首先,将空气传播和潘多拉TRVC进行比较,以评估机载TRVC的不确定性,并建立潘多拉观察的空间代表性。发现潘多拉和空气传播TRVC之间的171巧合是高度相关的(R2 = 0.92和1.03的斜率),具有高颞和/或空间可变性的个体差异。这些参考测量(Pandora和Airborge)是关于时间覆盖和空间代表性的互补性。 Pandora光谱仪可以提供连续的长期测量,但在直接阳光模式下操作时可能缺乏面积表示性。空中光谱仪通常仅在短时间内部署,但是它们的观察结果更加空间地代表卫星测量的卫星测量,通过在整个Tropomi像素上检索250m×250m的亚像素分辨率的添加能力。因此,空气传播的数据与Tropomi测量更相关(R2 = 0.96),而不是Pandora测量与rootomi(R2 = 0.84)。 Tropomi和参考测量之间的最大异常值似乎在明亮的城市场景中源于太空粗糙的优先表面反射率(0.5°)。在这项工作中,这导致在无云场景期间,有时的云场景受到对流层压力检索的误差影响的影响,影响到对流层空气质量因子的计算。该因素导致Tropomi TRVC的高偏差为4%-11%。除了这些云影响的积分之外,Tropomi在6月至9月的Listos TimeFrame期间的整体低偏差为19%-33%,2018年。这部分低偏压是由TM5-MP模型的粗糙度输入引起的;用12km北美模型 - 社区多尺度空气质量(Namcmaq)分析的替换这些简档导致TRVC增加12%-14%。即使通过这种改进,Tropomi-Namcmaq TRVC也具有7%-19%的低偏差,表明在空气质量因子计算中的先验假设中所需的改进。将来的工作应该探索先验输入的额外影响,以进一步评估rootomi中剩余的低偏差使用这些数据集。
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