Cargando…

The contribution of transport and chemical processes on coastal ozone and emission control strategies to reduce ozone

The interaction between transport and chemistry is pivotal for local ozone (O(3)) concentration, especially for a coastal region where the upstream sources might change diurnally. In the current emission control policy, most pollutants, such as particulate matter, SO(2), NOx, and CO, decrease while...

Descripción completa

Detalles Bibliográficos
Autores principales: Lien, Justin, Hung, Hui-Ming
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8545683/
https://www.ncbi.nlm.nih.gov/pubmed/34729439
http://dx.doi.org/10.1016/j.heliyon.2021.e08210
Descripción
Sumario:The interaction between transport and chemistry is pivotal for local ozone (O(3)) concentration, especially for a coastal region where the upstream sources might change diurnally. In the current emission control policy, most pollutants, such as particulate matter, SO(2), NOx, and CO, decrease while the annual O(3) trend might increase due to the complex feedbacks of precursors. In this study, we investigate the influence of transport upon the wintertime O(3) diurnal trend over ZuoYing Kaohsiung, an urban coastal site in southern Taiwan, by constructing a two-dimensional numerical model coupling both physical mechanisms and core chemical processes and provide a feasible emission control strategy. The transport process (i.e., import vs. export) for the daytime is determined using the Leighton Ratio (Φ), the ratio of O(3)-production over O(3)-loss rate, under the pseudo-steady-state condition. Φ shows a deviation of -9 to +13% from the photo-stationary state, and experiences a transition from import effect before 10:15 to weakening import or net export effect afterward associated with a net O(3) production as sea breeze starts developing. The significantly higher Φ derived from observation than from simulation by a factor of 1.35 might be resulted from the over-reported NO(2) due to NOy contribution on the NO(2) measurement, and the influence of aerosol and cloud possibly reducing ∼30% on applied NO(2) photolysis rate constant, associated with aerosol optical depth of 0.75 ± 0.15 and single scattering albedo of 0.85 ± 0.15. In this studied NOx-saturated regime, the addition of sea breeze convergence over the land enhances the maximal O(3) by ∼10%, mainly due to the O(3) accumulation (∼88%). Furthermore, the ozone isopleth analysis as a function of non-methane hydrocarbons and NOx emissions provides an achievable strategy to decrease both maximum daily ozone and the increment of ozone from morning to maximum by reducing hydrocarbons and NOx emissions, which can also eliminate the additional nitrate contribution on the aerosols.