HAZE-TO-FOG TRANSFORMATION DURING A LONG LASTING,LOW VISIBILITY EPISODE IN NANJING

被引:1
|
作者
张舒婷 [1 ]
牛生杰 [1 ]
机构
[1] Key Laboratory of Meteorological Disaster,Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters,Nanjing University of Informati
基金
中国国家自然科学基金;
关键词
haze; fog; transformation; meteorological elements;
D O I
10.16555/j.1006-8775.2016.S1.007
中图分类号
X51 [大气污染及其防治]; P427.2 [能见度、浑浊度];
学科分类号
0706 ; 070601 ; 070602 ;
摘要
Haze-to-fog transformation during a long lasting,low visibility episode was examined using the observations from a comprehensive field campaign conducted in Nanjing,China during 4-9 December 2013.In this episode,haze was transformed into fog and the fog lasted for dozens of hours.The impacts of meteorological factors such as wind,temperature(T) and relative humidity(RH) on haze,transition and fog during this episode were investigated.Results revealed significant differences between haze and fog days,due to their different formation mechanisms.Comparison was made for boundary-layer conditions during hazy days,haze-to-fog days and foggy days.Distributions of wind speed and wind direction as well as synoptic weather conditions around Nanjing had determinative impacts on the occurrences and characteristics of haze and fog.Weakened southerly wind in southern Nanjing resulted in high concentration of pollutants,and haze events occurred frequently during the study period.The wind speed was less than 1 m sin the haze event,which resulted in a stable atmospheric condition and weak dispersion of the pollutants.The height of the temperature inversion was about 400 m during the period.The inversion intensity was weak and the temperature-difference was 4℃ kmor less in haze,while the inversion was stronger,and temperature-difference was about 6℃ km,approaching the inversion layer intensity in the fog event.Haze event is strongly influenced by ambient RH.RH values increased,which resulted in haze days evidently increased,suggesting that an increasing fraction of haze events be caused by hygroscopic growth of aerosols,rather than simply by high aerosol loading.When RH was above 90%,haze aerosols started to be transformed from haze to fog.This study calls for more efforts to control emissions to prevent haze events in the region.
引用
收藏
页码:67 / 77
页数:11
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