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Influence of Arctic Oscillation abnormalities on spatio-temporal haze distributions in China

机译:北极涛动异常对中国时空雾度分布的影响

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摘要

This study investigates the impact of Arctic Oscillation (AO) abnormalities on the haze days in China for 57 winters from 1961 to 2017. The results reveal that that AO abnormalities mainly affected meteorological conditions and haze pollution in northern and central China, while their impact on the southeast coastal and Guangdong-Guangxi regions is not significant. During years with an abnormally high AO index (AOI) in winter, the number of haze days increased in northern and central China, especially in the Shanxi-Shandong-Hebei-Beijing-Tianjin and Hubei-Hunan-Henan-Jiangxi regions, while the number of haze days decreased during years of abnormally low AOI. When in the years of abnormally high AOI, the weakening of the East Asian trough caused the decrease of the meridional circulation and the increase of zonal winds compared with normal years. Furthermore, the weakening of the Siberian high pressure and the enhancement of the westerly circulation affected several meteorological factors, including the boundary layer height, surface temperature, wind speeds, and precipitations. These changes effectively inhibited the development of low-level vertical motion and the vertical diffusion of pollutants in the air, leading to the accumulation of haze pollution. The situation was the opposite for low AOI years, but the impact on the meteorological conditions was relatively weak compared to that during high AOI years. The impacts of the regional characteristics of AO abnormalities on the haze days are also investigated in this study.
机译:本研究调查了1961-2017年北极涛动(AO)异常对中国57个冬季的霾天的影响。结果表明,AO异常主要影响中国北部和中部的气象条件和霾污染,但对中国的影响东南沿海和粤广地区不显着。在冬季冬季AO指数异常高的年份,中国北部和中部的雾霾天数增加,尤其是山西-山东-河北-北京-天津和湖北-湖南-河南-江西地区。在异常低AOI的年份中,雾霾天数减少。当AOI异常高的年份时,与正常年份相比,东亚海槽的减弱导致子午环流的减少和纬向风的增加。此外,西伯利亚高压的减弱和西风环流的增强影响了一些气象因素,包括边界层高度,地表温度,风速和降水。这些变化有效地抑制了低水平垂直运动的发展以及空气中污染物的垂直扩散,导致了雾霾污染的积累。低AOI年份情况相反,但与高AOI年份相比,对气象条件的影响相对较弱。这项研究还研究了AO异常的区域特征对雾霾天的影响。

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