4.7 Article

Effect of land uses and wind direction on the contribution of local sources to airborne pollen

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 538, Issue -, Pages 672-682

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.scitotenv.2015.08.074

Keywords

Aeropalynology; Pollen spectrum; Urban green areas; Vegetation; Meteorological variables

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The interpretation of airborne pollen levels in cities based on the contribution of the surrounding flora and vegetation is a useful tool to estimate airbone allergen concentrations and, consequently, to determine the allergy risk for local residents. This study examined the pollen spectrum in a city in central Spain (Guadalajara) and analysed the vegetation landscape and land uses within a radius of 20 km in an attempt to identify and locate the origin of airborne pollen and to determine the effect of meterological variables on pollen emission and dispersal. The results showed that local wind direction was largely responsible for changes in the concentrations of different airborne pollen types. The land uses contributing most to airbone pollen counts were urban green spaces, through only 0.1% of the total surface area studied, and broadleaved forest which covered 5% of the study area. These two types of land use together accounted for 70% of the airbone pollen. Crops, scrubland and pastureland, though covering 80% of the total surface area, contributed only 18.6% to the total pollen count, and this contribution mainly consisted of pollen from Olea and herbaceous plants, including Poaceae, Urticaceae and Chenopodiaceae-Amaranthaceae. Pollen from ornamental species were mainly associated with easterly (Platanus), southerly (Cupressaceae) and westerly (Cupressaceae and Platanus) winds from the areas where the city's largest parks and gardens are located, Quercus pollen was mostly transported by winds blowing in from hol-oak stands on the eastern edge of the city. The highest Populus pollen counts were associated with easterly and westerly winds blowing in from areas containing rivers and streams. The airbone pollen counts generally rose with increasing temperature, solar radiation and hours of sunlight, all of which favour pollen release. In contrast, pollen counts declined with increased relative humidity and rainfall, which hinder airbone pollen transport. (C) 2015 Elsevier B.V. All rights reserved.

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