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Seasonal variations in physical characteristics of aerosol particles at the King Sejong Station, Antarctic Peninsula

机译:南极半岛世宗国王站气溶胶颗粒物理特征的季节性变化

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摘要

Seasonal variability in the physical characteristics of aerosol particlessampled from the King Sejong Station in the Antarctic Peninsula wasinvestigated over the period between March 2009 and February 2015. Clearseasonal cycles for the total particle concentration (CN) were observed. Themean monthly concentration of particles larger than 2.5 nm (CN) washighest during the austral summer, with an average value of1080.39 ± 595.05 cm, and lowest during the austral winter, witha mean value of 197.26 ± 71.71 cm. The seasonal patterns in theconcentrations of cloud condensation nuclei (CCN) and CN coincide, with bothconcentrations being at a minimum in winter and maximum in summer. Themeasured CCN spectra were approximated by fitting a power-law functionrelating the number of CCN for a given supersaturation (SS) to each SS value,with fitting coefficients and . The values for varied from6.35 to 837.24 cm, with a mean of 171.48 ± 62.00 cm.The values for ranged from 0.07 to 2.19, with a mean of0.41 ± 0.10. In particular, the values during the australsummer were higher than those during the winter, indicating that aerosolparticles are more sensitive to SS changes during summer. Furthermore, theannual mean hygroscopicity parameter, , was estimated as0.15 ± 0.05, for a SS of 0.4 %. The effects of the origin andpathway travelled by the air mass on the physical characteristics of theaerosol particles were also determined. The modal diameter of aerosolparticles originating in the South Pacific Ocean showed a seasonal variationvarying from 0.023 µm in winter to 0.034 µm in summer forthe Aitken mode, and from 0.086 µm in winter to 0.109 µmin summer for the accumulation mode.
机译:在2009年3月至2015年2月期间,调查了从南极半岛国王世宗站采样的气溶胶颗粒的物理特征的季节性变化。观察到总颗粒物浓度(CN)的季节清楚。在南方夏季,大于2.5 nm(CN)的微粒的每月平均浓度最高,平均值为1080.39±595.05 cm,而在南方冬季则最低,平均值为197.26±71.71 cm。云凝结核(CCN)和CN的浓度的季节模式一致,冬季的最低浓度和夏季的最高浓度。通过将幂函数与给定的过饱和度(SS)相关的CCN数量与每个SS值拟合,来拟合测得的CCN光谱,并具有拟合系数和。值从6.35到837.24 cm不等,平均值为171.48±62.00 cm。范围从0.07到2.19不等,平均值为0.41±0.10。尤其是,南澳大利亚夏季期间的值高于冬季期间的值,表明气溶胶颗粒在夏季对SS变化更敏感。此外,当SS为0.4%时,年平均吸湿性参数估计为0.15±0.05。还确定了气团行进的起点和路径对气溶胶颗粒物理特性的影响。起源于南太平洋的气溶胶颗粒的模态直径呈现季节变化,从冬季的0.023μm到夏季的Aitken模式为0.034μm,从冬季的0.086μm到累积模式的夏季为0.109μmmin。

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