English
 
Help Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT
  Mobile MAX-DOAS observations of tropospheric NO2 and HCHO during summer over the Three Rivers’ Source region in China

Cheng, S., Cheng, X., Ma, J., Xu, X., Zhang, W., Lv, J., et al. (2022). Mobile MAX-DOAS observations of tropospheric NO2 and HCHO during summer over the Three Rivers’ Source region in China. Atmospheric Chemistry and Physics Discussions, 22. doi:10.5194/acp-2022-629.

Item is

Files

show Files

Locators

show
hide
Description:
-
OA-Status:
Gold

Creators

show
hide
 Creators:
Cheng, Siyang, Author
Cheng, Xinghong, Author
Ma, Jianzhong, Author
Xu, Xiangde, Author
Zhang, Wenqian, Author
Lv, Jinguang, Author
Bai, Gang, Author
Chen, Bing, Author
Ma, Siying, Author
Dörner, Steffen1, Author           
Donner, Sebastian1, Author           
Wagner, Thomas1, Author           
Affiliations:
1Satellite Remote Sensing, Max Planck Institute for Chemistry, Max Planck Society, ou_1826293              

Content

show
hide
Free keywords: -
 Abstract: The tropospheric concentrations of nitrogen dioxide (NO2) and formaldehyde (HCHO) have high spatio-temporal variability, and in situ observations of these trace gases are still scarce especially in remote background areas. We made four similar circling journeys of mobile MAX-DOAS measurements in the Three Rivers’ Source region over the Tibetan Plateau in summer (18–30 July) 2021 for the first time. The differential slant column densities (DSCDs) of NO2 and HCHO were retrieved from the measured spectra with very weak absorptions along the driving routes. The tropospheric NO2 and HCHO vertical column densities (VCDs) were calculated from their DSCDs by the geometric approximation method, and they were further filtered to form reliable data sets by eliminating the influences of sunlight shelters and vehicle’s vibration and bumpiness. The observational data show that the tropospheric NO2 and HCHO VCDs decreased with the increasing altitude of the driving route, whose background levels were 0.40 ×1015 molec·cm−2 for NO2 and 2.27 ×1015 molec·cm−2 for HCHO in July 2021 over the Three Rivers’ Source region. The NO2 VCDs show similar geographical distribution patterns between the different circling journeys, but the levels of the HCHO VCDs are different between the different circling journeys. The NO2 VCDs tended to have peak values in the early morning and late afternoon, while the diurnal variation pattern of HCHO VCDs changed with the driving route. The elevated NO2 VCDs along the driving routes were usually corresponding to enhanced transport emissions from the towns crossed. However, the spatial distributions of the HCHO VCDs depended significantly on natural and meteorological conditions, such as surface temperature. By comparing TROPOMI satellite products and mobile MAX-DOAS results, we found that TROPOMI is still unable to identify the fine-scale spatial variability in tropospheric NO2 and HCHO VCDs in the background atmosphere over the Tibetan Plateau. Our study provides valuable data sets and information of NO2 and HCHO over the Tibetan Plateau, benefitting the scientific community in investigating the evolution of atmospheric composition with high spatio-temporal resolution in the background atmosphere at high altitudes, validating and improving the satellite products over mountain terrains, and evaluating the model’s ability in simulating atmospheric chemistry over the Tibetan Plateau.

Details

show
hide
Language(s): eng - English
 Dates: 2022-09-26
 Publication Status: Published online
 Pages: 36
 Publishing info: -
 Table of Contents: -
 Rev. Type: -
 Identifiers: DOI: 10.5194/acp-2022-629
 Degree: -

Event

show

Legal Case

show

Project information

show

Source 1

show
hide
Title: Atmospheric Chemistry and Physics Discussions
  Abbreviation : Atmos. Chem. Phys. Discuss.
Source Genre: Journal
 Creator(s):
Affiliations:
Publ. Info: -
Pages: - Volume / Issue: 22 Sequence Number: - Start / End Page: - Identifier: ISSN: 1680-7367
CoNE: https://pure.mpg.de/cone/journals/resource/111076360006006