Spectroscopy and Spectral Analysis, Volume. 42, Issue 7, 2039(2022)

Study on Vertical Distribution of Atmospheric HONO in Winter Based on Multi-Axis Differential Absorption Spectroscopy

Figures & Tables(8)
(a) Experimental setup of MAX-DOAS, (b) MAX-DOAS instrument and Observation site
Example of deconvolution of the DOAS spectrum in evaluation (a) O4, (b) NO2 and (c) HONO slant column densities of 2°elevation spectrum at 9:00 (Local Time) in December 9, 2017Bule lines represent the absorption signal and red lines represent the fit signal
A totally average daveraging kernel of (a) aerosol, (b) NO2 and (c) HONO at 09:00 (Local Time) on December 8, 2017The thin line represents the average nucleus connection curve, and the different colors represent different selected height layers (both 200 m are taken as one layer). The thick bmack solid line represents the envelope obtained by the inversion
The near-surface concentration (a) and vertical columndensity(b) of NO2 and HONO the first line of each figure is the profile of NO2 and HONO. The second line shows the time series for the ratio of HONO to NO2; And the third line is the time series of the AQI data released by the National Control Site named Dongpu ReservoirThe red dashed box indicates the deletion of MAX-DOAS observation data due to rainy, and the red dashed oval box indicates the lack of data due to instrumental observations
Time series of HONO (a) and NO2 (b) VMRs in the height of 10, 50 and 100 m
(a) Temporal series profiles of NO2 and HONO VMRs for the period December 26—31, 2017; (b) The backward trajectories of winds from December 29 to December 31, 2017, simulated by the Hysplit model; (c) Wind rose during the entire pollution period
  • Table 1. Parameter settings used for spectral analysis using the Windoas for NO2, O4, HCHO and HONO

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    Table 1. Parameter settings used for spectral analysis using the Windoas for NO2, O4, HCHO and HONO

    ParameterSourceSpecies
    NO2O4HONO
    Fitting spectral range338~375 nm338~375 nm335~373 nm
    Cross sectionNO2 at 220 and 298 K[9]√ (only 298 K) Taylor term*: λδNO2δNO22
    O4 at 293 K[10]
    O3 at 223 and 243 K[11]
    HCHO at 297 K[12]
    HONO at 296 K[13]
    H2O[14]
    BrO at 223 K[15]
    RingCalculate with QDOAS
    Polynomial degree335
    Intensity offsetConstantConstantPolynomial of order 1
  • Table 2. Detection limits of VCD and VMR of NO2 and HONO inversion by MAX-DOAS

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    Table 2. Detection limits of VCD and VMR of NO2 and HONO inversion by MAX-DOAS

    气体VCD检测限
    /(molecules·cm-2)
    VMR检测限
    /ppb
    数据保留量
    /%
    NO24.0×10130.15100.0
    HONO1.3×10130.0595.7
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. Study on Vertical Distribution of Atmospheric HONO in Winter Based on Multi-Axis Differential Absorption Spectroscopy[J]. Spectroscopy and Spectral Analysis, 2022, 42(7): 2039

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Paper Information

Category: Orginal Article

Received: May. 25, 2021

Accepted: --

Published Online: Nov. 16, 2022

The Author Email:

DOI:10.3964/j.issn.1000-0593(2022)07-2039-08

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