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African dust outbreaks over the western Mediterranean Basin: 11-year characterization of atmospheric circulation patterns and dust source areas

机译:地中海西部盆地非洲的粉尘暴发:大气环流模式和粉尘源区域的11年表征

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The occurrence of African dust outbreaks over different areas of the westernMediterranean Basin were identified on an 11-year period (2001–2011). Themain atmospheric circulation patterns causing the transport of African airmasses were characterized by means of an objective classification methodologyof atmospheric variable fields. Next, the potential source areas of mineraldust, associated to each circulation pattern were identified by trajectorystatistical methods. Finally, an impact index was calculated to estimate theincidence of the African dust outbreaks produced during each circulationpattern, in the areas of study.Four circulation types were obtained (I–IV) and three main potentialsource areas of African dust were identified (Western Sahara and Morocco;Algeria; northeastern Algeria and Tunisia). The circulation pattern I(24% of the total number of episodic days) produced the transport of dustmainly in summer from Western Sahara, southern Morocco and Tunisia. Thecirculation pattern IV (33%) brings dust mainly from areas of northernand southern Algeria in summer and autumn, respectively. The circulationpattern II (31%) favored the transport of dust predominantly fromnorthern Algeria, both in spring and summer. Finally, the circulation type III was the less frequently observed (12%). It occurred mainly in springand with less intensity in winter, carrying dust from Western Sahara andsouthern Morocco.Our findings point out that the most intense episodes over the westernMediterranean Basin were produced in the summer period by the circulationtype I (over the western side of the Iberian Peninsula) and the circulationtype IV (over the central and eastern sides of the Iberian Peninsula and theBalearic Islands).
机译:在为期11年(2001-2011年)的时间段内,确定了在地中海盆地西部不同地区发生的非洲沙尘暴爆发。利用大气可变场的客观分类方法,对引起非洲气团运输的主要大气环流模式进行了表征。接下来,通过轨迹统计方法确定了与每种循环模式相关的潜在矿物质源区域。最后,在研究区域中,计算了一个影响指数,以估计每种循环模式下非洲尘埃暴发的发生率。 获得了四种循环类型(I–IV)和三个非洲尘埃的主要潜在来源地区被确定(西撒哈拉和摩洛哥;阿尔及利亚;东北阿尔及利亚和突尼斯)。循环模式I(占总发作天数的24%)主要在夏季从西撒哈拉,摩洛哥南部和突尼斯运送了尘埃。 IV型循环(33%)分别在夏季和秋季带来了来自阿尔及利亚北部和南部地区的粉尘。 II型(31%)的循环模式有利于春季和夏季主要从阿尔及利亚北部运送灰尘。最后,循环类型III较少见(12%)。它主要发生在春季,冬季强度较小,携带着来自西撒哈拉和摩洛哥南部的尘埃。 我们的研究结果指出,地中海盆地西部最强烈的事件是夏季由I型环流造成的。伊比利亚半岛的西侧)和IV型环流(越过伊比利亚半岛和巴利阿里群岛的中部和东部)。

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