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Sea-land breeze in a coastal city and its effect on pollen transport

机译:沿海城市的海陆风及其对花粉运输的影响

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This paper presents a statistical study of the sea-land breeze in Mar del Plata (Argentina) to characterize the periods of the year when the breeze affects pollen transport, particularly the dispersion of airborne Poaceae pollen between urban and rural areas. In order to analyse the sea breeze circulation, hourly data from coastal, urban and rural meteorological stations were used. The effect of the sea breeze on the particulate matter was analysed from syncronic hourly airborne pollen records from an urban and a rural area. A sea-land breeze appeared between spring and early autumn in the hours of greatest diurnal warming. Results showed that the surface wind direction most probably associated with this phenomenon is NE and E, the time of occurrence shifting to new directions following the counter-clockwise rotation, according to theoretical models for the Southern Hemisphere. Poaceae emission takes place in the morning, during the hours of maximum insolation. However, after the occurrence of the breeze, a rise in pollen concentration between 2000 hours and 0200 hours is detected because of pollen reentrainment brought about by air recirculation. The results showed that breeze transport brings a regional component to pollen assemblage.
机译:本文对马德普拉塔(阿根廷)的海陆风进行了统计研究,以表征一年中微风影响花粉运输的时期,特别是空中的禾本科花粉在城乡之间的分散。为了分析海风环流,使用了沿海,城市和农村气象站的每小时数据。根据城市和农村地区每小时一次的同步空中花粉记录,分析了海风对颗粒物的影响。在最大的昼间升温期间,春季和秋季初之间出现了海风。结果表明,根据南半球的理论模型,与该现象有关的表面风向最可能是NE和E,发生时间随着逆时针旋转而转移到新的方向。禾本科植物的排放发生在最大日照时间的早晨。然而,在微风发生后,由于空气再循环导致花粉重新夹带,因此检测到花粉浓度在2000小时至0200小时之间升高。结果表明,微风的运输给花粉组合带来了区域性的影响。

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