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北极黄河站秋季气团传输影响下大气气溶胶数谱分布特征
引用本文:沈小静,孙俊英,张养梅,李卫军,迟建伟,张璐,樊如霞.北极黄河站秋季气团传输影响下大气气溶胶数谱分布特征[J].冰川冻土,2016,38(3):604-610.
作者姓名:沈小静  孙俊英  张养梅  李卫军  迟建伟  张璐  樊如霞
作者单位:中国气象科学研究院 灾害天气国家重点实验室/中国气象局 大气化学重点开放实验室,北京,100081;中国气象科学研究院 灾害天气国家重点实验室/中国气象局 大气化学重点开放实验室,北京 100081;中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室,甘肃 兰州 730000;山东大学环境研究院,山东 济南,250100
基金项目:中国极地科学战略研究基金项目(20140310);国家自然科学基金(41175113;41405132)
摘    要:2013年9月在北极黄河站开展了气溶胶数谱(10~400 nm)的短期观测实验.数浓度小时平均值主要出现在300~400 cm~(-3),平均值为350 cm~(-3),高于新奥尔松Zeppelin全球大气本底站及环北极海洋大气7-9月航测报道的浓度.大气气溶胶的三个模态(核模态、爱根核模态和积聚模态)数浓度平均分别为35、122和193 cm~(-3).观测期间没有发生新粒子生成事件,平均数谱分布呈现双模态的分布特征,模态峰值分别出现在30 nm和115 nm,由积聚模态主导.平均数谱分布的几何中值粒径出现在约100~110 nm.从单颗粒分析结果来看,观测期间黄河站地区大气气溶胶主要以海盐气溶胶为主,但是在来自挪威海域和北欧大陆的气团影响下,也观测到煤烟颗粒、富硫颗粒物和含碳颗粒物等人为气溶胶.

关 键 词:北极  大气气溶胶  数谱分布  后向轨迹  单颗粒分析

The characteristics of atmospheric aerosol particle number size distribution in Arctic Yellow River Station influenced by long-range transport of autumn air mass
SHEN Xiaojing,SUN Junying,ZHANG Yangmei,LI Weijun,CHI Jianwei,ZHANG Lu,FAN Ruxia.The characteristics of atmospheric aerosol particle number size distribution in Arctic Yellow River Station influenced by long-range transport of autumn air mass[J].Journal of Glaciology and Geocryology,2016,38(3):604-610.
Authors:SHEN Xiaojing  SUN Junying  ZHANG Yangmei  LI Weijun  CHI Jianwei  ZHANG Lu  FAN Ruxia
Abstract:Measurement of particle number size distribution(PNSD)in the size range of 10~400 nm was car-ried out at Yellow River Station in Arctic in September 2013. During the measurement,it was found that the val-ue of hourly mean number concentration of 300~400 cm-3 presented most frequently,with a mean value of 350 cm-3. The number concentration was much higher than the values reported by the study at Zeppelin Station in Ny-?lesund and the cruises in the central Arctic between July and September. The number concentration of the three modes(nucleation mode,Aitken mode and accumulation mode)was 35,122 and 193 cm-3,respectively. There was no new particle formation event observed during the measurement. The PNSD was characterized by bimodal distribution,with one mode peaking at 30 nm and the other at 115 nm,respectively. The PNSD was dominated by the accumulation mode,with the geometric mean diameter of 100~110 nm. Based on the analysis of the indi-vidual particle samples,it was found that the chemical component during the measurement was mainly contribut-ed by the sea salt particles. However,when air mass from Norwegian Sea and Northern Europe became domi-nant,the soot particles,sulfur-rich and carbonaceous particles were also observed,revealing the influence by the anthropogenic emissions.
Keywords:Arctic  atmospheric aerosols  particle number size distribution  back trajectory  individual particle analysis
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