05 Jul 2022
05 Jul 2022
Status: a revised version of this preprint is currently under review for the journal ACP.

Impacts of reductions in non-methane short-lived climate forcers on future climate extremes and the resulting population exposure risks in Asia

Yingfang Li1, Zhili Wang1,2, Yadong Lei1, Huizheng Che1, and Xiaoye Zhang1 Yingfang Li et al.
  • 1State Key Laboratory of Severe Weather and Key Laboratory of Atmospheric Chemistry of CMA, Chinese Academy of Meteorological Sciences, Beijing, 100081, China
  • 2Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing, 210044, China

Abstract. Non-methane short-lived climate forcers (SLCFs), including aerosols, ozone, and their precursors, are important climate forcings and primary air pollutants. Stringent SLCF emissions controls to mitigate air pollution have been implemented by various governments, which will substantially impact the future climate. We investigate the changes in future climate extremes and resulting population exposure risks in Asia during 2031–2050 in response to non-methane SLCF emissions reductions using multi-model ensemble (MME) simulations under two scenarios (SSP3-7.0 and SSP3-7.0-lowNTCF) with different air quality control measures from the Aerosol and Chemistry Model Intercomparison Project (AerChemMIP), which is endorsed by Coupled Model Intercomparison Project phase 6 (CMIP6). The MME results show that future reductions in non-methane SLCF emissions lead to an increase of 0.23 W m-2 in global annual mean effective radiative forcing, thereby magnifying the greenhouse gas (GHG)-induced global surface warming by 0.19 K during 2031–2050. The additional warming caused by the non-methane SLCF reductions increases the regional average temperature on the hottest days (TXx) by 0.3 K, the percentage of warm days (TX90p) by 4.8 %, the number of tropical nights (TR) by 1.7 days, the warm spell duration (WSDI) by 1.0 days, the number of heavy precipitation days (R10) by 1.3 days, the maximum consecutive 5-day precipitation (RX5day) by 0.8 mm, and the total wet-day precipitation (R95p) by 16.4 mm during 2031–2050. For temperature extremes, the largest regional increases of TXx, TX90p, and WSDI occur in northern India (NIN) and northern China (NC). Relatively large increases in TR are predicted in NC and the Sichuan Basin (SCB), reaching 5.1 days and 4.9 days, respectively. For precipitation extremes, the regional changes are greatest in southern China (SC), particularly southwestern China (SWC), where reductions of non-methane SLCF emissions increases R10 by 3.0 days, RX5day by 2.2 mm, and R95p by 39.5 mm. Moreover, the populations exposed to temperature and precipitation extremes increase most sharply in NIN, reaching (32.2 ± 11.4) × 107 person-days and (6.7 ± 7.8) × 106 person-days during 2031–2050, respectively, followed by NC and SCB. Our results highlight the significant impacts of non-methane SLCF reductions on future climate extremes and related exposure risks in Asia, which are comparable to the impact associated with increased GHG forcing in some regions.

Yingfang Li et al.

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2022-422', Anonymous Referee #1, 19 Jul 2022
    • AC1: 'Reply on RC1', yingfang Li, 22 Sep 2022
  • RC2: 'Comment on acp-2022-422', Anonymous Referee #2, 11 Aug 2022
    • AC2: 'Reply on RC2', yingfang Li, 22 Sep 2022

Yingfang Li et al.

Yingfang Li et al.


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Short summary
Since few studies accessed the impacts of future combined reductions of aerosols, ozone, and their precursors on future climate change, especially at regional scale. We use models with interactive representation of tropospheric aerosols and atmospheric chemistry schemes to quantify the impact of their reductions on Asian climate. Our results suggest that their reductions will exacerbate the warming effect caused by GHGs, increasing future climate extremes and associated exposure risks.