2016
DOI: 10.1038/srep34408
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A paradox for air pollution controlling in China revealed by “APEC Blue” and “Parade Blue”

Abstract: A series of strict emission control measures were implemented in Beijing and surrounding regions to ensure good air quality during the 2014 Asia-Pacific Economic Cooperation (APEC) summit and 2015 Grand Military Parade (Parade), which led to blue sky days during these two events commonly referred to as “APEC Blue” and “Parade Blue”. Here we calculated Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) and Ozone Monitoring Instrument (OMI) NO2 and HCHO results based on well known DOAS trace gas … Show more

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Cited by 82 publications
(88 citation statements)
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References 63 publications
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“…Vertical distribution profiles of aerosols and trace gases are also important for AMF calculations. In this study, trace gas profiles (e.g., O 3 , NO 2 , SO 2 , and HCHO) and vertical profiles of pressure and temperature are taken from the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem) simulations for AMF calculations (Liu et al, 2016). Atmospheric profiles obtained from the model simulation were then interpolated in both spatial and temporal dimensions to MAX-DOAS measurements' location and time for AMF calculation.…”
Section: Q Hong Et Al: Ship-based Max-doas Measurementsmentioning
confidence: 99%
See 1 more Smart Citation
“…Vertical distribution profiles of aerosols and trace gases are also important for AMF calculations. In this study, trace gas profiles (e.g., O 3 , NO 2 , SO 2 , and HCHO) and vertical profiles of pressure and temperature are taken from the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem) simulations for AMF calculations (Liu et al, 2016). Atmospheric profiles obtained from the model simulation were then interpolated in both spatial and temporal dimensions to MAX-DOAS measurements' location and time for AMF calculation.…”
Section: Q Hong Et Al: Ship-based Max-doas Measurementsmentioning
confidence: 99%
“…The local overpass time of OMI is between 13:40 and 13:50 (local time) on the ascending node. In this study, USTC's OMI tropospheric NO 2 product is used, which is developed based on OMI's primary product and has proven to be more suitable for the atmospheric conditions in China (Liu et al, 2016;Xing et al, 2017;Su et al, 2017). Slant column densities (SCDs) of NO 2 are retrieved by applying the DOAS fit to OMI spectra (data source: OMI Level 1B VIS Global Radiances Data product (OML1BRVG), https://disc.gsfc.nasa.…”
Section: Omi Satellite Observationsmentioning
confidence: 99%
“…Vertical distribution profiles of aerosols and trace gases are also important for the AMF calculation. In this study, trace gas profiles (e.g., O 3 , NO 2 , SO 2 , and HCHO) and vertical profiles of pressure and temperature are taken from WRFChem simulations for AMF calculations (Liu et al, 2016). Aerosol extinction coefficients in the lowest 2 km of the 170 troposphere were taken from the Mie lidar measurements while aerosols above 2 km were not considered in the radiative transfer simulations.…”
Section: Determination Of the Tropospheric Vcd 145mentioning
confidence: 99%
“…In this study, USTC's OMI tropospheric NO 2 product is used (Liu et al, 2016). Slant column densities (SCDs) of NO 2 are retrieved by applying the DOAS fit to OMI spectra.…”
Section: Omi Satellite Observationsmentioning
confidence: 99%
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