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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Spatial and seasonal variations of sand-dust events and their relation to atmospheric conditions and vegetation cover in semi-arid regions of central Iran
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Spatial and seasonal variations of sand-dust events and their relation to atmospheric conditions and vegetation cover in semi-arid regions of central Iran

机译:沙尘事件的空间和季节变化及其与伊朗中部半干旱地区大气条件和植被覆盖的关系

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摘要

Atmospheric conditions and physical characteristics of the earth surface have an important effect on the spatiotemporal variations of sand-dust events. The main objective of the present study was to investigate the effect of these variables on the seasonal variation of these events in semi-arid regions of Central Iran Zone (CIZ). The Ridge Regression (RR) method was used to analyze the relationship between seasonal variations of precipitation, surface winds speed, air temperature, and Enhanced Vegetation Index (EVI) with Dust Storm Index (DSI) for two different periods (2001-2008 and 2009-2016). The dusty winds direction around the study area was also determined using the dust roses. The results showed that the annual DSI changes in the study area had a week incremental trend with a rate of 0.07/8 yrs in the previous period while it followed a strong increasing trend with a rate of 0.22/8 yrs in the latter period. It was also found that the activity of sand-dust storms in the second period was greater than the first period, especially in the border region of Iran and Turkmenistan. According to RR analysis, DSI had a significant positive association with the surface winds speed in the summer (beta = +0.48; p-value < 0.05) and the winter precipitation (beta = 0.3; p-value < 0.05) over the previous period. During this period, there was no significant relationship between the temperature and EVI with DSI in other seasons (pvalue > 0.05). In the second period, the surface winds speed was positively correlated with the DSI in the spring beta = + 2.04), summer (beta = + 2.6) and autumn (beta = + 2.08). The significant negative relationship between EVI and DSI changes was observed only in the spring season (beta = 0.7; p-value < 0.05). Our findings also indicated that dusty winds direction in the northeast, northwest, and southeast parts of the study area were from the northwest, southeast, and west, respectively. These findings can help to mitigate the negative consequences of dust emissions and improve the wind erosion management in semi-dry lands of CIZ.
机译:地球表面的大气条件和物理特征对沙尘事件的时空变化具有重要影响。本研究的主要目的是调查这些变量对伊朗半干旱地区(CIZ)的半干旱地区季节变化的影响。脊回归(RR)方法用于分析两次不同时期的沉淀,表面风速,空气温度,增强植被指数(EVI)的季节变化与增强植被指数(EVI)之间的关系(2001-2008和2009年-2016)。使用灰尘玫瑰也确定研究区域周围的尘土飞扬的风向。结果表明,研究区的年度DSI变化有一周的增量趋势,前一期的速度为0.07 / 8年,而后期随后的趋势率为0.22 / 8年。还发现,第二个时期的沙尘暴活动大于第一时期,特别是在伊朗和土库曼斯坦的边境地区。根据RR分析,DSI在夏季(β= +0.48; p值<0.48)和冬季沉淀(β= 0.3; p值<0.05)中具有显着的阳性关系。 。在此期间,温度和EVI与其他季节的温度和EVI之间没有显着的关系(PValue> 0.05)。在第二个时段中,​​表面风速与Springβ= + 2.04的DSI呈正相关),夏季(β= + 2.6)和秋季(Beta = + 2.08)。仅在春季(β= 0.7; p值<0.05)只观察到EVI和DSI变化之间的显着负相关关系。我们的调查结果表明,研究区东北部,西北和东南部的东北部和东南部的东南部地区的尘土风向的风向分别来自西北,东南,西部。这些调查结果可以帮助减轻尘埃排放的负面后果,并改善CIZ半干旱地区的风蚀管理。

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