2018
DOI: 10.1038/s41598-018-24366-3
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New positive feedback mechanism between boundary layer meteorology and secondary aerosol formation during severe haze events

Abstract: Severe haze events during which particulate matter (PM) increases quickly from tens to hundreds of microgram per cubic meter in 1–2 days frequently occur in China. Although it has been known that PM is influenced by complex interplays among emissions, meteorology, and physical and chemical processes, specific mechanisms remain elusive. Here, a new positive feedback mechanism between planetary boundary layer (PBL), relative humidity (RH), and secondary PM (SPM) formation is proposed based on a comprehensive fie… Show more

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Cited by 101 publications
(95 citation statements)
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“…Reduced surface downward shortwave radiation due to ARI shows a linear relationship with surface PM 2.5 concentrations ( figure S1(a)). This linear relationship is consistent with observations of surface PM 2.5 concentration and solar radiation in Beijing as shown by Liu et al (2018). Decreases in PBLH due to ARI follow a quadratic relationship with surface PM 2.5 concentrations ( figure S1(b)), reflecting a positive feedback between the two.…”
Section: Weakened Ari Effects Due To Emission Reductionssupporting
confidence: 90%
See 1 more Smart Citation
“…Reduced surface downward shortwave radiation due to ARI shows a linear relationship with surface PM 2.5 concentrations ( figure S1(a)). This linear relationship is consistent with observations of surface PM 2.5 concentration and solar radiation in Beijing as shown by Liu et al (2018). Decreases in PBLH due to ARI follow a quadratic relationship with surface PM 2.5 concentrations ( figure S1(b)), reflecting a positive feedback between the two.…”
Section: Weakened Ari Effects Due To Emission Reductionssupporting
confidence: 90%
“…Additional positive feedback can be caused by changes in other meteorological variables, such as RH. Decreases in downward solar radiation tend to decrease surface temperature and increase RH ( figure S1(c)), leading to conditions favorable for secondary aerosol formation (Liu et al 2018).…”
Section: Weakened Ari Effects Due To Emission Reductionsmentioning
confidence: 99%
“…For BLH values above 800 m, the PD remains constant, that is, the influence of the boundary layer on PM concentrations stagnates (Liu et al, ). Mean modeled PM10 concentrations increase slightly in conditions with very high BLH (>2,000 m).…”
Section: Resultsmentioning
confidence: 99%
“…This similarity is encouraging and proves the robustness of the modeling approach, since both studies use ERA-Interim BLH in a comparable geographic setting. For BLH values above ∼800 m, the PD remains constant, that is, the influence of the boundary layer on PM concentrations stagnates (Liu et al, 2018). Mean modeled PM10 concentrations increase slightly in conditions with very high BLH (>2,000 m).…”
Section: Blh and Capementioning
confidence: 95%
“…Aerosols change weather and climate via the following pathways: they absorb and scatter solar and thermal radiation to alter the radiative balance of the earth-atmosphere system (Gao et al, 2019b;Liu et al, 2011;Jia et al, 2018), which is referred to as direct effects, and they serve as cloud condensation nuclei (CCN) and/or ice nuclei (IN) to modify cloud properties, which is referred to as indirect effects (Haywood and Boucher, 2000). The suppression of cloud convection induced by direct effects of absorbing aerosols is known as the semidirect effect Lohmann and Feichter, 2005).…”
Section: Introductionmentioning
confidence: 99%