Articles | Volume 18, issue 19
https://doi.org/10.5194/acp-18-13969-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-18-13969-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
02 Oct 2018
Research article |
| 02 Oct 2018
| 02 Oct 2018
Daytime HONO, NO2 and aerosol distributions from MAX-DOAS observations in Melbourne
Robert G. Ryan
CORRESPONDING AUTHOR
School of Earth Sciences, University of Melbourne, Melbourne, Australia
ARC Centre of Excellence for Climate System Science, Sydney, Australia
Steve Rhodes
Bureau of Meteorology, Melbourne, Australia
Matthew Tully
Bureau of Meteorology, Melbourne, Australia
Stephen Wilson
School of Chemistry, University of Wollongong, Wollongong, Australia
Nicholas Jones
School of Chemistry, University of Wollongong, Wollongong, Australia
Udo Frieß
Institute for Environmental Physics, University of Heidelberg, Heidelberg, Germany
Robyn Schofield
School of Earth Sciences, University of Melbourne, Melbourne, Australia
ARC Centre of Excellence for Climate System Science, Sydney, Australia
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Cited
37 citations as recorded by crossref.
- Global and Regional Patterns of Soil Nitrous Acid Emissions and Their Acceleration of Rural Photochemical Reactions D. Wu et al. 10.1029/2021JD036379
- A new insight into the vertical differences in NO2 heterogeneous reaction to produce HONO over inland and marginal seas C. Xing et al. 10.5194/acp-23-5815-2023
- Stereoscopic hyperspectral remote sensing of the atmospheric environment: Innovation and prospects C. Liu et al. 10.1016/j.earscirev.2022.103958
- Seasonal Characteristics of HONO Variations in Seoul during 2021~2022 J. Gil et al. 10.5572/KOSAE.2023.39.3.308
- Identifying the wintertime sources of volatile organic compounds (VOCs) from MAX-DOAS measured formaldehyde and glyoxal in Chongqing, southwest China C. Xing et al. 10.1016/j.scitotenv.2019.136258
- Ground-based vertical profile observations of atmospheric composition on the Tibetan Plateau (2017–2019) C. Xing et al. 10.5194/essd-13-4897-2021
- Exploration of the atmospheric chemistry of nitrous acid in a coastal city of southeastern China: results from measurements across four seasons B. Hu et al. 10.5194/acp-22-371-2022
- HONO Measurement in Seoul during Summer 2018 and its Impact on Photochemistry J. Gil et al. 10.5572/KOSAE.2020.36.5.579
- Diagnosis of Ozone Formation Sensitivities in Different Height Layers via MAX‐DOAS Observations in Guangzhou H. Lin et al. 10.1029/2022JD036803
- Vertical characteristics and potential sources of aerosols over northeast China using ground-based MAX-DOAS C. Gao et al. 10.1016/j.apr.2023.101691
- Observations of the vertical distributions of summertime atmospheric pollutants in Nam Co: OH production and source analysis C. Xing et al. 10.5194/acp-24-10093-2024
- Vertical distributions of tropospheric SO2 based on MAX-DOAS observations: Investigating the impacts of regional transport at different heights in the boundary layer Q. Hong et al. 10.1016/j.jes.2020.09.036
- Time-Dependent Uptake of O3 and NO2 on Methane Soot Coatings under the Conditions of Their Competitive Adsorption V. Zelenov & E. Aparina 10.1134/S1990793121050225
- A relaxed eddy accumulation (REA) LOPAP system for flux measurements of nitrous acid (HONO) L. von der Heyden et al. 10.5194/amt-15-1983-2022
- Spatiotemporal Distribution, Sources, and Impact on Atmospheric Oxidation of Reactive Nitrogen Oxides in the North China Plain Agricultural Regions in Summer S. Wei et al. 10.3390/rs16173192
- Vertical characteristics of NO2 and HCHO, and the ozone formation regimes in Hefei, China B. Ren et al. 10.1016/j.scitotenv.2022.153425
- Investigation of the Formation and Photolysis Characteristics of HONO and their Effect on O3 Formation in the Daejeon and Seoul Atmosphere during Winter N. Kim et al. 10.5572/KOSAE.2024.40.3.302
- HONO, Particulate Nitrite, and Snow Nitrite at a Midlatitude Urban Site during Wintertime Q. Chen et al. 10.1021/acsearthspacechem.9b00023
- Identification of ozone sensitivity for NO2 and secondary HCHO based on MAX-DOAS measurements in northeast China J. Xue et al. 10.1016/j.envint.2021.107048
- Measurement report: MAX-DOAS measurements characterise Central London ozone pollution episodes during 2022 heatwaves R. Ryan et al. 10.5194/acp-23-7121-2023
- Observations of HONO and its precursors between urban and its surrounding agricultural fields: The vertical transports, sources and contribution to OH C. Xing et al. 10.1016/j.scitotenv.2023.169159
- Fast Secondary Aerosol Formation in Residual Layer and Its Impact on Air Pollution Over Eastern China X. Zhou et al. 10.1029/2023JD038501
- Comparison of formaldehyde tropospheric columns in Australia and New Zealand using MAX-DOAS, FTIR and TROPOMI R. Ryan et al. 10.5194/amt-13-6501-2020
- Characteristics of HONO and its impact on O3 formation in the Seoul Metropolitan Area during the Korea-US Air Quality study J. Gil et al. 10.1016/j.atmosenv.2020.118182
- Two-dimensional monitoring of air pollution in Madrid using a Multi-AXis Differential Optical Absorption Spectroscopy two-dimensional (MAXDOAS-2D) instrument D. Garcia-Nieto et al. 10.5194/amt-14-2941-2021
- A CNN-SVR model for NO2 profile prediction based on MAX-DOAS observations: The influence of Chinese New Year overlapping the 2020 COVID-19 lockdown on vertical distributions of tropospheric NO2 in Nanjing, China X. Tian et al. 10.1016/j.jes.2023.09.007
- Inter-comparison of MAX-DOAS measurements of tropospheric HONO slant column densities and vertical profiles during the CINDI-2 campaign Y. Wang et al. 10.5194/amt-13-5087-2020
- Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China H. Lin et al. 10.3390/rs12193193
- Ozone profiles without blind area retrieved from MAX-DOAS measurements and comprehensive validation with multi-platform observations X. Ji et al. 10.1016/j.rse.2022.113339
- Surface ozone exceedances in Melbourne, Australia are shown to be under NOx control, as demonstrated using formaldehyde:NO2 and glyoxal:formaldehyde ratios R. Ryan et al. 10.1016/j.scitotenv.2020.141460
- Budget of atmospheric nitrous acid (HONO) during the haze and clean periods in Shanghai: Importance of heterogeneous reactions J. Feng et al. 10.1016/j.scitotenv.2023.165717
- Vertical profiles of the transport fluxes of aerosol and its precursors between Beijing and its southwest cities Q. Hu et al. 10.1016/j.envpol.2022.119988
- Evolution of the vertical structure of air pollutants during winter heavy pollution episodes: The role of regional transport and potential sources Q. Hong et al. 10.1016/j.atmosres.2019.05.016
- Vertical distributions of atmospheric HONO and the corresponding OH radical production by photolysis at the suburb area of Shanghai, China S. He et al. 10.1016/j.scitotenv.2022.159703
- Unveiling the effect of O2 on the photochemical reaction of NO2 with polycyclic aromatic hydrocarbons W. Yang et al. 10.1007/s11356-023-30289-y
- Amplified role of potential HONO sources in O<sub>3</sub> formation in North China Plain during autumn haze aggravating processes J. Zhang et al. 10.5194/acp-22-3275-2022
- Heterogeneous photochemical uptake of NO2 on the soil surface as an important ground-level HONO source W. Yang et al. 10.1016/j.envpol.2020.116289
37 citations as recorded by crossref.
- Global and Regional Patterns of Soil Nitrous Acid Emissions and Their Acceleration of Rural Photochemical Reactions D. Wu et al. 10.1029/2021JD036379
- A new insight into the vertical differences in NO2 heterogeneous reaction to produce HONO over inland and marginal seas C. Xing et al. 10.5194/acp-23-5815-2023
- Stereoscopic hyperspectral remote sensing of the atmospheric environment: Innovation and prospects C. Liu et al. 10.1016/j.earscirev.2022.103958
- Seasonal Characteristics of HONO Variations in Seoul during 2021~2022 J. Gil et al. 10.5572/KOSAE.2023.39.3.308
- Identifying the wintertime sources of volatile organic compounds (VOCs) from MAX-DOAS measured formaldehyde and glyoxal in Chongqing, southwest China C. Xing et al. 10.1016/j.scitotenv.2019.136258
- Ground-based vertical profile observations of atmospheric composition on the Tibetan Plateau (2017–2019) C. Xing et al. 10.5194/essd-13-4897-2021
- Exploration of the atmospheric chemistry of nitrous acid in a coastal city of southeastern China: results from measurements across four seasons B. Hu et al. 10.5194/acp-22-371-2022
- HONO Measurement in Seoul during Summer 2018 and its Impact on Photochemistry J. Gil et al. 10.5572/KOSAE.2020.36.5.579
- Diagnosis of Ozone Formation Sensitivities in Different Height Layers via MAX‐DOAS Observations in Guangzhou H. Lin et al. 10.1029/2022JD036803
- Vertical characteristics and potential sources of aerosols over northeast China using ground-based MAX-DOAS C. Gao et al. 10.1016/j.apr.2023.101691
- Observations of the vertical distributions of summertime atmospheric pollutants in Nam Co: OH production and source analysis C. Xing et al. 10.5194/acp-24-10093-2024
- Vertical distributions of tropospheric SO2 based on MAX-DOAS observations: Investigating the impacts of regional transport at different heights in the boundary layer Q. Hong et al. 10.1016/j.jes.2020.09.036
- Time-Dependent Uptake of O3 and NO2 on Methane Soot Coatings under the Conditions of Their Competitive Adsorption V. Zelenov & E. Aparina 10.1134/S1990793121050225
- A relaxed eddy accumulation (REA) LOPAP system for flux measurements of nitrous acid (HONO) L. von der Heyden et al. 10.5194/amt-15-1983-2022
- Spatiotemporal Distribution, Sources, and Impact on Atmospheric Oxidation of Reactive Nitrogen Oxides in the North China Plain Agricultural Regions in Summer S. Wei et al. 10.3390/rs16173192
- Vertical characteristics of NO2 and HCHO, and the ozone formation regimes in Hefei, China B. Ren et al. 10.1016/j.scitotenv.2022.153425
- Investigation of the Formation and Photolysis Characteristics of HONO and their Effect on O3 Formation in the Daejeon and Seoul Atmosphere during Winter N. Kim et al. 10.5572/KOSAE.2024.40.3.302
- HONO, Particulate Nitrite, and Snow Nitrite at a Midlatitude Urban Site during Wintertime Q. Chen et al. 10.1021/acsearthspacechem.9b00023
- Identification of ozone sensitivity for NO2 and secondary HCHO based on MAX-DOAS measurements in northeast China J. Xue et al. 10.1016/j.envint.2021.107048
- Measurement report: MAX-DOAS measurements characterise Central London ozone pollution episodes during 2022 heatwaves R. Ryan et al. 10.5194/acp-23-7121-2023
- Observations of HONO and its precursors between urban and its surrounding agricultural fields: The vertical transports, sources and contribution to OH C. Xing et al. 10.1016/j.scitotenv.2023.169159
- Fast Secondary Aerosol Formation in Residual Layer and Its Impact on Air Pollution Over Eastern China X. Zhou et al. 10.1029/2023JD038501
- Comparison of formaldehyde tropospheric columns in Australia and New Zealand using MAX-DOAS, FTIR and TROPOMI R. Ryan et al. 10.5194/amt-13-6501-2020
- Characteristics of HONO and its impact on O3 formation in the Seoul Metropolitan Area during the Korea-US Air Quality study J. Gil et al. 10.1016/j.atmosenv.2020.118182
- Two-dimensional monitoring of air pollution in Madrid using a Multi-AXis Differential Optical Absorption Spectroscopy two-dimensional (MAXDOAS-2D) instrument D. Garcia-Nieto et al. 10.5194/amt-14-2941-2021
- A CNN-SVR model for NO2 profile prediction based on MAX-DOAS observations: The influence of Chinese New Year overlapping the 2020 COVID-19 lockdown on vertical distributions of tropospheric NO2 in Nanjing, China X. Tian et al. 10.1016/j.jes.2023.09.007
- Inter-comparison of MAX-DOAS measurements of tropospheric HONO slant column densities and vertical profiles during the CINDI-2 campaign Y. Wang et al. 10.5194/amt-13-5087-2020
- Validation of Water Vapor Vertical Distributions Retrieved from MAX-DOAS over Beijing, China H. Lin et al. 10.3390/rs12193193
- Ozone profiles without blind area retrieved from MAX-DOAS measurements and comprehensive validation with multi-platform observations X. Ji et al. 10.1016/j.rse.2022.113339
- Surface ozone exceedances in Melbourne, Australia are shown to be under NOx control, as demonstrated using formaldehyde:NO2 and glyoxal:formaldehyde ratios R. Ryan et al. 10.1016/j.scitotenv.2020.141460
- Budget of atmospheric nitrous acid (HONO) during the haze and clean periods in Shanghai: Importance of heterogeneous reactions J. Feng et al. 10.1016/j.scitotenv.2023.165717
- Vertical profiles of the transport fluxes of aerosol and its precursors between Beijing and its southwest cities Q. Hu et al. 10.1016/j.envpol.2022.119988
- Evolution of the vertical structure of air pollutants during winter heavy pollution episodes: The role of regional transport and potential sources Q. Hong et al. 10.1016/j.atmosres.2019.05.016
- Vertical distributions of atmospheric HONO and the corresponding OH radical production by photolysis at the suburb area of Shanghai, China S. He et al. 10.1016/j.scitotenv.2022.159703
- Unveiling the effect of O2 on the photochemical reaction of NO2 with polycyclic aromatic hydrocarbons W. Yang et al. 10.1007/s11356-023-30289-y
- Amplified role of potential HONO sources in O<sub>3</sub> formation in North China Plain during autumn haze aggravating processes J. Zhang et al. 10.5194/acp-22-3275-2022
- Heterogeneous photochemical uptake of NO2 on the soil surface as an important ground-level HONO source W. Yang et al. 10.1016/j.envpol.2020.116289
Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
Nitrous acid (HONO) plays a crucial role in the self-cleansing capacity of the atmosphere but its formation mechanisms and spatial distributions are not well understood. This paper presents spectroscopic measurements of HONO, NO2 and aerosol measurements from Melbourne, Australia. HONO levels are at a maximum in the middle of the day, which is unprecedented for an urban area, and these measurements provide evidence for the existence of a strong ground-based, daytime nitrogen oxide source.
Nitrous acid (HONO) plays a crucial role in the self-cleansing capacity of the atmosphere but...
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