摘要
基于无锡市2008-2011年酸雨观测资料，利用功率谱分析、后向轨迹和聚类分析方法，研究了无锡市酸雨的变化特征，分析了气象因素对酸雨的影响，探讨了1500m高度的气团移动路径特征。结果表明：2008～2011年，无锡市酸雨pH值呈现逐年递增趋势，而且酸雨逐月pH值、逐月弱酸雨和强酸雨频率分别存在不同的周期性变化；酸雨酸性随降水量增加表现为先增强后减弱，但夏季降水与酸雨pH值的相关性并不显著；春季相对湿度与酸雨pH值呈现显著负相关，夏季气温则与酸雨pH值呈显著正相关；各季节1500m高度的轨迹存在一定差异，春冬季无锡市受内陆气团影响为主，夏秋季西太平洋水汽输送作用明显。总体而言，江浙赣和西太平洋是无锡酸雨前体物的主要来源地。
Based on the observation data of acid rain in Wuxi during 2008--2011,we analyzed the temporal characteristics of acid rain, the relationship with meteorological conditions and the characteristics of 1500 m moving path to investigate the effect of diffusion of acid precursor on acid rain with power spectrum analysis,backward trajectory and clustering analysis. The results showed that the annual value of pH appeared an increasing trend in Wuxi.The frequency of strong acid rain decreased year by year,while that of weak acid rain increased.The frequency in summer and autumn was low while that in spring was high. The acidity of rain was weak in June and July while strong in September. The large-value and low-value months of strong acid rain frequency were March and July, respectively. The large-value and low-value months of weak acid rain frequency were August and September, respectively. The monthly pH and the frequencies of weak acid rain and strong acid rain had different periodic change.We found that the monthly pH had low-frequency variation of 5-6 months.We also found that the frequencies of weak and strong acid rain had high-frequency variation of 2.1 and 2.5.The acidity of rain increased first and then decreased with the increasing precipitation, because the concentration o~ acid substance was high at the initial stage of raining while it was lower with raining.But the relationship between the precipitation of summer and the pH of acid rain was not significant while it＇s significant in spring,autumn and winter.There was significant negative correlation between the relative humidity of spring and the value of pH because the ascending of relative humidity strengthened the hydration of acid ions and the acidity of rain was higher with the absorption and collision of rain.There was significant positive correlation between atmospheric temperature of summer and the value of pH because hyperthermia helps vertical convection and the concentration of acid precursor became lower with horizontal migration of 1500 m.The simulations of backward traiectories showed that the trajectories of 1 500 m in different seasons are different,but Jiangsu,Zhejiang,Jiangsu are the main sources of acid precursor.These domains were polluted severely and they were typical high-value regions of and .The paths of simulations of backward trajectories were short relatively and the air mass moves slow in these regions.It did not help the dilution and diffusion of pollutants,but the effect of vapor transportation eased the acidity of rain from Western Pacific in summer and autumn. In general, there is relationship between rain in Wuxi and acid precursor of Jiangsu, Zhejiang and Jiangxi in spring, summer and autumn.The trajectory of transportation on pollutants is long and it helps the dilution and diffusion of pollutants,so the pH of the rain in winter is larger than the pH in spring.
出处
《长江流域资源与环境》
CAS
CSSCI
CSCD
北大核心
2014年第1期89-94,共6页
Resources and Environment in the Yangtze Basin
关键词
酸雨
PH值
气象条件
后向轨迹
acid rain
the value of pH
meteorological condition
backward trajectory
作者简介
钱吴钟（1985-），男，硕士，主要研究方向为气象及其环境效应．E-mail：wuxiqhz@163．com
