Dual effects of the winter monsoon on haze‐fog variations in eastern China

Abstract

Abstract Previous studies have revealed a negative correlation between the East Asian winter monsoon and wintertime haze‐fog events in China. The winter monsoon reduces haze‐fog by advecting away aerosol particles and supplying clean air through cold waves. However, it is found that the frequency of haze‐fog events on subseasonal time scales displays no correlation with typical winter monsoon indices. The results show that the accumulating and maintaining effects of calm weather related to the Siberian High, which is also a part of the monsoon circulation system, are equally important for the development of haze‐fog events during winter. Correlation analysis indicates that subseasonal variations in haze‐fog are closely related to the intensity of the Siberian High ( r = 0.49). The Siberian High may increase the occurrence of haze‐fog events by reducing the near surface wind speed and enhancing the stratification stability. To quantify the contribution of these diverse effects of the winter monsoon on the variations in haze‐fog events, we analyzed haze‐fog events during periods of cold wave activity and calm weather separately and contrasted the relative contributions of these two effects on different time scales. On the subseasonal scale, the effect of the Siberian High was 2.0 times that of cold waves; on the interannual scale, the effect of cold waves was 2.4 times that of the Siberian High. This study reveals the dual effects of the East Asian winter monsoon on wintertime haze‐fog variations in eastern China and provides a more comprehensive understanding of the relationship between the monsoon and haze‐fog events.