摘要
根据临安区域本底站观测资料分析结果得出,中国中纬度地区秋、冬季O3及其前体物NOx等浓度偏高,可以对农作物和地表生态系统产生影响。观测结果表明:近地层大气O3浓度主要决定于地面总辐射量控制下的光化学反应过程;O3的生成受到前体物NOx的控制,但O3与NOx存在着明显的非线性关系。从PEM-WESTA和B的实验及1995年的观测资料表明,O3的生成效率随着NOx浓度的增大而减小。尽管O3的生成速率秋季比冬季的大,但由于秋季较高的NOx抑制了过氧基的生成,因此冬季O3的累积量几乎可以和秋季相比拟。在临安观测的NMHC和NOx的比值比国外同纬度地区测值要大。这说明在临安本底站O3的光化学生成中,NMHC不是控制物种。从而提示我们,在这些季节临安O3光化学产物能够被NOx浓度所控制。中美大气化学联合考察(PEM-WEST-B)实验期间,台湾省的卡盯站SO2的平均浓度为0.29ppb,O3的平均浓度为42.2ppb,可以认为此值为低纬度海岛的本底值。1994年PEM-WEST-B实验期间临安站的观测资料和台湾省的卡盯站资料相比,临安站SO2的浓度约为卡盯站SO2浓度的50倍左右,从而可以看出人类活动对大气本底的显著影?
ccording to measurement result at Linan,we can address some conclusions. The O3 and its precursor NOx concentrations are higher in autumn and spring in middle latitude of China.Such higher O3 has an adverse effect on crops and economics system.O3 concentration in boundary layer is determined by photochemical process controlled by surface global radiation.There is an obviously nonlinear relationship between O3 and NOx.The data taken from period of PEMWESTA and B 1995 shows that:The production efficiency of O3 decrease with NOx concentration increasing.Althouht the efficiency of O3 production in autumn is higher than that in winter,because of the higher NOx in autumn limited (HO2) production,so the accumulated O3 concentration in winter almost is comparable with that of in autumn.The ratio of NMHC to NOx at Linan is higher than that at abroad similar latitude.It seems that O3 photochemical production may be comtroled by NOx at Linan in these seasons.(There for it prompts that because of the NMHC produced by nature resources is higher,so if we want to control O3 concentration,we should contrlo NOx discharge.)The average SO2 concentration at Kangting in Taiwan is 0.29 ppb during PEMWESTB.The SO2 concentration at Linan is 50 times higher than that at Kangting during PEMWESTB in 1994.This value may be the representive of background SO2 at island in low latitude.It is clearly that the human action effects obviously on the value of atmospheric background.
出处
《气象学报》
CSCD
北大核心
1998年第4期467-475,共9页
Acta Meteorologica Sinica