title: [Seasonal Dynamics of Airborne Pollens and Its Relationship with Meteorological Factors in Beijing Urban Area].
abstract: The seasonal dynamics of airborne pollens and their relationship with meteorological conditions, which are considered to be important factors for appropriate construction of urban green system and reliable prevention of tropic pollinosis, were investigated in Beijing urban area. The airborne pollens were monitored from December 31st 2011 to December 31st 2012 by Burkard volumetric trap, and the data were analyzed. The results revealed that: (1) In 2012 the pollen dispersion period lasted 238 days from March 17 to November 18th, accounting for 65% of the year. There were two peaks of pollen amount in air, which occurred from March to May and from August to October, respectively. In the spring peak, tree pollens such as Oleaceae, Populus and Salix pollens were the dominant, accounting for 53% of the total annual pollens, while in the autumn period, weed pollens such as Compositae, Chenopodiaceae and Amaranthaceae pollens made up about 40% of the annual total value; (2) The highly allergenic weeds pollens dominated in autumn, which caused a high incidence of tropic pollinosis; (3) The airborne pollen amount of Beijing urban area was significantly affected by meteorological condition like the wind speed, temperature, humidity, precipitation and so on; (4) When temperature ranged from OC to 15 degrees C, the pollen amount showed positive relation with temperature; while in the temperature range of 18 degrees C to 30 degrees C, it showed negative relation; (5) The average temperature of spring and autumn season in 2012 was 17 degrees C, and 79% of airborne pollens were detected in these two seasons. This temperature condition was conducive to the pollen dispersion. (6) The pollen amount showed negative relation with relative moisture between 20% and 50% and larger than 70%, while in the moisture range of 50% to 60%, it showed positive relation; (7) The wind speed smaller than 3 m x s(-1) was good to pollen distribution, when it was larger than 4 m x s(-1) or the wind lasted for a long time, the pollen amount in the air would decrease; (8) The pollen release was decreased by the rain. The above results can be helpful to forecast the pollen amount in the air. monitoring; pollen amount
authors.forename: Ling
authors.initials: L
authors.lastname: Meng
authors.forename: Xiao-ke
authors.initials: XK
authors.lastname: Wang
authors.forename: Zhi-yun
authors.initials: ZY
authors.lastname: Ouyang
authors.forename: Yu-fen
authors.initials: YF
authors.lastname: Ren
authors.forename: Qiao-huan
authors.initials: QH
authors.lastname: Wang
mesh_terms: D000485:Allergens / Q000032:analysis*; D027703:Amaranthaceae; D019659:Asteraceae; D000068476:Beijing; D019663:Chenopodiaceae; D008685:Meteorological Concepts; D011058:Pollen; D011891:Rain; D012621:Seasons; D013696:Temperature; D014919:Wind
chemical_list: D000485:Allergens