厄瓜多尔基多的高空间分辨率WRF-Chem模型

IF 4.4 Q3 ENGINEERING, ENVIRONMENTAL
Gabriela Mancheno and Héctor Jorquera
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引用次数: 0

摘要

WRF-Chem模式在厄瓜多尔基多以2公里的高水平分辨率应用于气体和气溶胶化学。之所以选择WRF-Chem,是因为它完全耦合了气象和化学过程,特别适合复杂地形和城市尺度的模拟。外域(32 km和8 km水平分辨率)采用EDGAR的排放清单,内域(2 km分辨率)采用局地排放估算作为初始估算。模拟的基准年为2018年,选择了4月和12月两个月。WRF-Chem的结果在基多大都市区的五个空气质量站进行了测试。为了减少模拟浓度与观测浓度之间的偏差,基多2011年CO、NOx、SO2和PM2.5的基线排放量约按1.5、0.75、0.30和3.0的因子进行调整,得出CO、NOx(以NO2当量表示)、SO2和PM2.5的年排放量分别为300、27、1.5和7.5千吨/年(千吨/年)。使用这些调整后的排放量运行的模型显示,CO、NOx、SO2和O3的性能良好(r ~ 0.4-0.8),但PM2.5的性能较低(r ~ 0.4-0.5),特别是在下午。这主要是由于低估了次生有机气溶胶的形成。生物源性VOC排放对臭氧和PM2.5的影响是正的,但影响很小(+ 3-8%),由于基多的环境PM2.5浓度相对较小,气溶胶辐射反馈的影响较小(~ - 0.5%)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

High spatial resolution WRF-Chem modeling in Quito, Ecuador†

High spatial resolution WRF-Chem modeling in Quito, Ecuador†

The WRF-Chem model was applied for gas and aerosol chemistry in Quito, Ecuador, at a high horizontal resolution of 2 km. WRF-Chem was chosen due to its full coupling of meteorological and chemical processes, which is particularly suitable for complex topography and urban-scale simulations. Emission inventories were taken from EDGAR for the outer domains (32 and 8 km horizontal resolution), and local emission estimates were used for the innermost domain (2 km resolution) as initial estimates. The base year of simulation was 2018, and two months were chosen: April and December. WRF-Chem results were tested at five air quality stations across the Quito metropolitan area. To reduce bias between modeled and observed concentrations, Quito 2011 baseline emissions for CO, NOx, SO2, and PM2.5 were adjusted by factors of 1.5, 0.75, 0.30 and 3.0 approximately, resulting in annual emission estimates of 300, 27, 1.5 and 7.5 kilotonnes per year (kton per year) for CO, NOx (expressed as NO2 equivalent), SO2 and PM2.5, respectively. The model run with these adjusted emissions showed good performance for CO, NOx, SO2, and O3 (r ∼0.4–0.8), but performance was lower for PM2.5 (r ∼0.4–0.5), particularly in the afternoon. This is ascribed mainly to an underestimation of secondary organic aerosol formation. The impact of biogenic VOC emissions on ozone and PM2.5 is positive but small (+3–8%), and the inclusion of aerosol radiative feedback is minor (∼−0.5%), because of the relatively small ambient PM2.5 concentrations in Quito.

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