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Variability of blowing dust weather frequency over semi-arid areas of China (Baicheng, Jilin Province) and relationships with climatic factors during 1951-2006

机译:1951-2006年中国半干旱地区(吉林省白城市)吹尘天气频率的变化及其与气候因子的关系

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We analyzed the variability of blowing dust weather frequency (BDWF) and patterns in climatic factors over Baicheng for the period 1951-2006 in this study. The data showed that blowing dust over Baicheng occurs intensively during the spring and shows significant inter-decadal variability. One of the main findings is that the occurrence of blowing dust has significantly decreased after the mid-1980s. The mean wind speed (WS), diurnal temperature range (DTR), relative humidity (RH) and precipitation at Baicheng during the spring show decreasing trends. The decreasing trends of the mean WS and DTR are significant at 99% confidence levels according to the t-test; the dataset also indicated a sharp decrease in WS occurred after the mid-1980s. The mean surface air temperature (SAT) escalated in a fluctuating manner during 1951-2006. BDWF at Baicheng was significantly related to local WS, SAT and DTR during the spring [correlation coefficients (CCs) are 0.41, -0.47 and 0.36, respectively]. The correlation between BDWF at Baicheng and selected climatic factors over the sand-dust source regions and transmission paths were also calculated. We found that BDWF is well correlated to the mean WS and SAT during the spring, with CCs of 0.45 and -0.48, respectively. The most likely causes for the dramatic decrease observed in BDWF after the mid-1980s were related to the adjustment of large-scale circulation patterns in response to a decrease of meridional temperature differences, the weakening of steering westerlies and the strengthening of downward motions that has occurred at the middle latitudes of eastern Eurasia in recent decades.
机译:本文分析了白城地区1951-2006年的吹尘天气频率(BDWF)和气候因子模式的变化。数据显示,春季白城上空扬尘密集,年代际变化显着。主要发现之一是1980年代中期以后吹尘的发生率显着下降。春季白城的平均风速(WS),昼夜温度范围(DTR),相对湿度(RH)和降水量呈下降趋势。根据t检验,平均WS和DTR的下降趋势在99%的置信水平上是显着的;该数据集还表明,1980年代中期之后WS急剧下降。在1951年至2006年期间,平均地面气温(SAT)呈波动上升。春季白城的BDWF与当地的WS,SAT和DTR显着相关[相关系数(CC)分别为0.41,-0.47和0.36]。还计算了白城的BDWF与沙尘源区和传输路径上选定气候因子之间的相关性。我们发现,BDWF与春季的平均WS和SAT密切相关,CC分别为0.45和-0.48。导致1980年代中期BDWF急剧下降的最可能原因与对子午温差减小,转向西风减弱和下沉运动加强的大环流模式的调整有关。最近几十年来发生在欧亚大陆东部中纬度地区。

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