Preprints
https://doi.org/10.5194/egusphere-2023-207
https://doi.org/10.5194/egusphere-2023-207
26 Jun 2023
 | 26 Jun 2023

The influences of El Niño–Southern Oscillation on tropospheric ozone in CMIP6 models

Thanh Le, Seon-Ho Kim, Jae-Yeong Heo, and Deg-Hyo Bae

Abstract. Ozone in the troposphere is a greenhouse gas and a pollutant, hence, additional understanding of the drivers of tropospheric ozone evolution is essential. The El Niño–Southern Oscillation (ENSO) is a main climate mode and may contribute to the variations of tropospheric ozone. Nevertheless, there is uncertainty regarding the causal influences of ENSO on tropospheric ozone under warming environment. Here, we investigated the links between ENSO and tropospheric ozone using Coupled Modeling Intercomparison Project Phase 6 (CMIP6) data over the period 1850–2014. Our results show that ENSO impacts on tropospheric ozone are primarily found over oceans, while the signature of ENSO over continents is largely nonsignificant. The response of ozone to ENSO may vary depending on specific air pressure levels in the troposphere. These responses are weak in the middle troposphere and are stronger in the upper and lower troposphere. Although there are biases in simulating the signature of ENSO on surface ozone, these signatures in the middle and upper troposphere appear to be more consistent across CMIP6 models. While the response of tropical tropospheric ozone to ENSO is in agreement with previous works, our results suggest that ENSO impacts on tropospheric ozone of the mid-latitude regions over the southern Pacific, Atlantic, and Indian oceans might be more significant than previously understood.

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Journal article(s) based on this preprint

04 Jun 2024
The influences of El Niño–Southern Oscillation on tropospheric ozone in CMIP6 models
Thanh Le, Seon-Ho Kim, Jae-Yeong Heo, and Deg-Hyo Bae
Atmos. Chem. Phys., 24, 6555–6566, https://doi.org/10.5194/acp-24-6555-2024,https://doi.org/10.5194/acp-24-6555-2024, 2024
Short summary
Thanh Le, Seon-Ho Kim, Jae-Yeong Heo, and Deg-Hyo Bae

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-207', Anonymous Referee #1, 11 Jul 2023
    • AC1: 'Reply on RC1', Thanh Le, 07 Dec 2023
  • RC2: 'Comment on egusphere-2023-207', Anonymous Referee #3, 13 Nov 2023
    • AC2: 'Reply on RC2', Thanh Le, 07 Dec 2023

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-207', Anonymous Referee #1, 11 Jul 2023
    • AC1: 'Reply on RC1', Thanh Le, 07 Dec 2023
  • RC2: 'Comment on egusphere-2023-207', Anonymous Referee #3, 13 Nov 2023
    • AC2: 'Reply on RC2', Thanh Le, 07 Dec 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Thanh Le on behalf of the Authors (07 Dec 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (19 Dec 2023) by Graciela Raga
RR by Anonymous Referee #3 (28 Dec 2023)
ED: Reconsider after major revisions (01 Mar 2024) by Graciela Raga
AR by Thanh Le on behalf of the Authors (30 Mar 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (22 Apr 2024) by Graciela Raga
AR by Thanh Le on behalf of the Authors (23 Apr 2024)

Journal article(s) based on this preprint

04 Jun 2024
The influences of El Niño–Southern Oscillation on tropospheric ozone in CMIP6 models
Thanh Le, Seon-Ho Kim, Jae-Yeong Heo, and Deg-Hyo Bae
Atmos. Chem. Phys., 24, 6555–6566, https://doi.org/10.5194/acp-24-6555-2024,https://doi.org/10.5194/acp-24-6555-2024, 2024
Short summary
Thanh Le, Seon-Ho Kim, Jae-Yeong Heo, and Deg-Hyo Bae
Thanh Le, Seon-Ho Kim, Jae-Yeong Heo, and Deg-Hyo Bae

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Short summary
We examined the links between El Niño–Southern Oscillation (ENSO) and tropospheric ozone (O3) using models’ data. Our results show that ENSO impacts on tropospheric O3 are mainly found over oceans, while the signature of ENSO over continents is largely unclear. These impacts in the mid-latitude regions over the southern hemisphere may be more significant than previously known. The responses of O3 to ENSO are weak in the middle troposphere and are stronger in the upper and lower troposphere.