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Spatio-Temporal Land Use Regression Modelling of Ozone Levels in Athens, Greece

机译:希腊雅典臭氧水平的时空土地利用回归模型

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Background and aims: Spatio-temporal methods have been developed for the estimation of concentrations of pollutants such as particulate matter (PM) and nitrogen dioxide (NO2) for application in epidemiological studies. A very limited number of city-specific spatio-temporal ozone (O3) models have been proposed recently. Our aim was to develop a spatio-temporal land use regression (LUR) model that estimates daily concentrations of O3, for the whole year, warm (April 1st to 30th September) and cold season (October 1st and 31st March), within the greater Athens area. Methods: We developed models using a semiparametric approach including linear and smooth functions of spatial and temporal covariates and a bivariate smooth thin plate function. The final set of explanatory variables was selected based on the adjusted-R2. We tested the final model in temporal and spatial terms following a leave-one out monitor approach. Results: The adjusted-R2 of the developed annual model was 0.76, while for the warm and cold season it was 0.70 and 0.71, respectively. The spatial terms in our annual model explained 32.9% and the temporal 63.2% of the variability in O3. There was no remaining temporal or spatial autocorrelation in the residuals. The adjusted-R2 in the leave-one-out cross validation was 0.73 for the annual model (warm: 0.65 and cold: 0.70). The developed models showed good validity when comparing predicted and observed measurements for the 2015 data. Conclusions: Spatio-temporal LUR modeling provides a useful tool for estimating 03 spatio-temporal variability with adequate accuracy for subsequent use in epidemiological studies.
机译:背景和目的:时空方法已经开发出来,用于估算污染物(例如颗粒物(PM)和二氧化氮(NO2))的浓度,用于流行病学研究。最近已经提出了数量非常有限的特定于城市的时空臭氧(O3)模型。我们的目标是建立一个时空土地利用回归(LUR)模型,以估算较大范围内全年,温暖(9月1日至30日)和寒冷季节(3月1日至3月31日)每天的O3浓度。雅典地区。方法:我们使用半参数方法开发了模型,包括空间和时间协变量的线性和平滑函数以及双变量平滑薄板函数。根据调整后的R2选择最终的解释变量集。我们采用了“留一法”监控方法,在时间和空间方面对最终模型进行了测试。结果:所开发的年度模型的调整后R2为0.76,而在温暖和寒冷季节的调整后R2分别为0.70和0.71。我们年度模型中的空间术语解释了O3的32.9%的时间变化和63.2%的时间变化。残差中没有剩余的时间或空间自相关。年度模型的留一法交叉验证中的调整后R2为0.73(温暖:0.65;寒冷:0.70)。当比较2015年数据的预测和观察到的测量值时,开发的模型显示出良好的有效性。结论:时空LUR建模为估算03时空变异性提供了一个有用的工具,具有足够的准确性,可用于随后的流行病学研究。

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