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Investigation of the diurnal pattern of the vertical distribution of pollen in the lower troposphere using LIDAR

机译:用LIDAR研究对流层下花粉垂直分布的日变化规律。

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The diurnal pattern of the vertical distribution of biogenic pollen in thelower troposphere was investigated by LIDAR. Meteorological data were takenat the ground. Pollen concentrations were measured at the surface using aBurkard 7-day-recording volumetric spore sampler. Aerosol extinctioncoefficients and depolarization ratios at 532 nm were obtained from LIDARmeasurements in spring (4 May–2 June) 2009 in Gwangju, South Korea. Linearvolume depolarization ratios varied between 0.08 and 0.14 and were observedonly during daytime (09:00–17:00 local time (LT)) during days of high pollenconcentration (4 to 9 May). Daily average pollen concentrations ranged1000–2500 cm?3 in the same period. The temporal evolution of thevertical distribution of the linear volume depolarization ratio showed aspecific diurnal pattern. Linear volume depolarization ratios of more than0.06, were measured near the surface in the morning. High depolarizationratios were detected up to 2 km aboveground between 12:00 and 14:00 LT,whereas high depolarization ratios were observed only close to the surfaceafter 17:00 LT. Low values of depolarization ratios (≤0.05) weredetected after 18:00 LT until the next morning. During the measurementperiod, the daily variations of the high depolarization ratios close to thesurface showed correlation to number concentration measurements of pollen.This finding suggests that high depolarization ratios could be attributed toenhanced pollen concentrations. The diurnal characteristics of the highvalues of depolarization ratios are thought to be closely associated withturbulent transport. Diurnal and vertical characteristics of pollen, ifmeasured continuously, could be used to improve the accuracy ofpollen-forecasting models via data assimilation studies.
机译:利用激光雷达研究了对流层下部生源花粉垂直分布的日变化规律。地面的气象数据。使用记录了7天的Burkard体积孢子取样器测量表面的花粉浓度。 2009年春季(5月4日至6月2日),韩国光州的LIDAR测量获得了532 nm处的气溶胶消光系数和去极化比。线性体积的去极化比在0.08和0.14之间变化,并且仅在高花粉浓度(5月4日至9日)的白天(当地时间09:00-17:00)观察到。同期平均日花粉浓度为1000-2500 cm ?3 。线性体积去极化比的垂直分布的时间演变表现出特定的昼夜模式。早晨在地面附近测得的线性体积消极化比大于0.06。在中午12:00至14:00之间,在距地面2 km处检测到高去极化比,而在17:00 LT之后仅在接近地面的地方观察到了高去极化比。在18:00 LT直到第二天早晨,检测到的去极化比值较低(≤0.05)。在测量期间,接近表面的高去极化率的日变化与花粉的数量浓度测量值相关。这一发现表明,高去极化率可以归因于花粉浓度的增加。去极化比的高值的昼夜特征被认为与湍流运输密切相关。如果连续测量花粉的昼夜和垂直特征,则可以通过数据同化研究来提高花粉预测模型的准确性。

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