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Analysis on the decadal scale variation of the dust storm in North China

机译:华北沙尘暴年代际变化分析

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In this paper, the temporal variation characteristics of the dust storm in North China are investigated. Based on power spectrum analysis and wavelet analysis, 1956-1970 and 1985-1999 are chosen as the high-frequency and low-frequency dust storm decades respectively. Analysis results clearly show that the spring and wintertime anomalous atmospheric circulation between these two decades are significantly different. Compared with the former decade, there are a strengthened polar vortex, enhanced westerlies near 50°N, and a weak East Asian major though in the winter of the latter decade. The north and center parts of the Siberian high and the Aleutian low become weak. The southerly and easterly wind anomalies appear over the north and east parts of China, which implies the weakening of East Asian winter monsoon. Meanwhile, northern China experiences warmer winters and wetter springs, which are in favor of the weakening of dust storm intensity in North China. There are significant out-of-phase relationships between dust frequency and wintertime westerly intensity, as well as between dust frequency and Arctic Oscillation. It is also found that the frequency of dust weather is strongly related to winter-springtime East Asian monsoon intensity.
机译:本文研究了华北沙尘暴的时空变化特征。根据功率谱分析和小波分析,分别选择1956-1970年和1985-1999年为高频和低频沙尘暴十年。分析结果清楚地表明,这两个十年之间的春季和冬季异常大气环流有显着差异。与前十年相比,尽管在后十年的冬季,极地涡旋增强,北纬50°附近的西风增强,东亚专业减弱。西伯利亚高压和阿留申低压的北部和中部变弱。中国北部和东部地区出现南风和东风异常,这意味着东亚冬季风减弱。同时,中国北方的冬季和春季较温暖,这有利于华北地区沙尘暴强度的减弱。尘埃频率与冬季西风强度之间以及尘埃频率与北极涛动之间存在明显的异相关系。还发现,沙尘天气的频率与冬春季东亚季风强度密切相关。

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