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Long-term variations in PM(2.5) concentrations under changing meteorological conditions in Taiwan

With emission control efforts, the PM(2.5) concentrations and PM(2.5) exceedance days (daily mean PM(2.5) concentrations >35 µg m(−3)) show an apparent declining trend from 2006–2017. The PM(2.5) concentrations increase from the northern to southern part of western Taiwan, and reductions in the P...

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Detalles Bibliográficos
Autores principales: Cheng, Fang-Yi, Hsu, Chia-Hua
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6488571/
https://www.ncbi.nlm.nih.gov/pubmed/31036848
http://dx.doi.org/10.1038/s41598-019-43104-x
Descripción
Sumario:With emission control efforts, the PM(2.5) concentrations and PM(2.5) exceedance days (daily mean PM(2.5) concentrations >35 µg m(−3)) show an apparent declining trend from 2006–2017. The PM(2.5) concentrations increase from the northern to southern part of western Taiwan, and reductions in the PM(2.5) concentration generally decrease from northern to southern part of western Taiwan. Thus, mitigation of the PM(2.5) problem is less effective in southwestern Taiwan than in other regions in Taiwan. Analysis of a 39-year ERA-interim reanalysis dataset (1979–2017) reveals a weakening of the East Asian winter monsoon, a reduction in northeasterly (NE) monsoonal flow, and a tendency of enhanced stably stratified atmospheric structures in Taiwan and the surrounding area. The observed surface wind speed also presents a long-term decline. We can conclude that the long-term PM(2.5) variations in Taiwan are mainly associated with changes in local anthropogenic emissions and modulated by short-term yearly variations due to strong haze events in China. In southwestern Taiwan, the long-term trend of PM(2.5) reductions is possibly offset by worsening weather conditions, as this region is situated on the leeside of the mountains and often subject to stagnant wind when under the influence of NE monsoonal flow.