Acta Optica Sinica, Volume. 44, Issue 24, 2401005(2024)

Spectral Remote Sensing of NO2 Vertical Profile Variation Difference in Beijing During Major Events and Holidays

Jian Chen1, Chengzhi Xing2、*, Jinan Lin2, and Cheng Liu1,2
Author Affiliations
  • 1Department of Precision Machinery and Precision Instrumentation, University of Science and Technology of China, Hefei 230026, Anhui , China
  • 2Key Laboratory of Environmental Optics & Technology, Chinese Academy of Sciences, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei 230031, Anhui , China
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    Figures & Tables(11)
    MAX-DOAS station
    Correlations between MAX-DOAS NO2 volume fraction and CNEMC NO2 mass concentration
    Time series of NO2 volume fraction at 0‒200 m, 400‒600 m, and 800‒1000 m height layers from June 2020 to May 2022
    Seasonal averaged vertical profiles of NO2 volume fraction, and the shadow represents standard deviation. (a) Spring; (b) summer; (c) autumn; (d) winter
    Averaged diurnal variations of NO2 volume fraction in different seasons. (a) Spring; (b) summer; (c) autumn; (d) winter
    Averaged diurnal variations of boundary layer height in different seasons
    Averaged vertical profiles and averaged diurnal variations of NO2 volume fraction. (a)(b) Weekdays; (c)(d) Saturday; (e)(f) Sunday
    Averaged vertical profiles and averaged diurnal variations of NO2 volume fraction. (a)(b) All observation periods; (c)(d) holidays; (e)(f) major events
    WPSCF distribution of NO2 in the bottom layer (0‒20 m). (a) February 2021; (b) February 2022
    • Table 1. Detailed parameter settings of DOAS inversion for NO2

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      Table 1. Detailed parameter settings of DOAS inversion for NO2

      ParameterData source
      NO2Vandaele et al.[32], 1998, 294 K
      HCHOMeller and Moortgat[33], 2000, 297 K
      O3Serdyuchenko et al.[34], 2014, 223 K
      O3Serdyuchenko et al.[34] , 2014, 243 K
      O4Thalman and Volkamer[35], 2013, 293 K
      BrOFleischmann et al.[36], 2004, 223 K
      RingRing spectra calculated with QDOAS, according to Chance and Spurr[37], 1997
      Polynomial degreeOrder5
      Intensity offsetConstant
    • Table 2. Major events and holidays during the observation period

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      Table 2. Major events and holidays during the observation period

      TypeEvent/holidayTime period

      Major

      event

      Winter Olympics2022‒02‒04—02‒20
      Paralympic Winter Games2022‒03‒04—03‒13
      HolidayDragon Boat Festival2020‒06‒25—06‒27; 2021‒06‒12—12‒14
      Qingming Festival2021‒04‒03—04‒05; 2022‒04‒03—04‒05
      International Labor Day2021‒05‒01—05‒05; 2022‒04‒30—05‒04
      Mid-Autumn Festival2021‒09‒19—09‒21
      National Day2020‒10‒01—10‒08; 2021‒10‒01—10‒07
      New Year’s Day2021‒01‒01—01‒03; 2022‒01‒01—01‒03
      Spring Festival2021‒02‒11—02‒17; 2022‒01‒31—02‒06
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    Jian Chen, Chengzhi Xing, Jinan Lin, Cheng Liu. Spectral Remote Sensing of NO2 Vertical Profile Variation Difference in Beijing During Major Events and Holidays[J]. Acta Optica Sinica, 2024, 44(24): 2401005

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    Paper Information

    Category: Atmospheric Optics and Oceanic Optics

    Received: Feb. 18, 2024

    Accepted: May. 27, 2024

    Published Online: Dec. 17, 2024

    The Author Email: Xing Chengzhi (xingcz@aiofm.ac.cn)

    DOI:10.3788/AOS240638

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