首页> 外文期刊>Physio - Geo: geographie physique et environnement: Physio-Géo >Ampleur de la sécheresse dans le bassin d'alimentation du barrage Meffrouche (Nord-Ouest de l'Algérie)
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Ampleur de la sécheresse dans le bassin d'alimentation du barrage Meffrouche (Nord-Ouest de l'Algérie)

机译:Meffrouche大坝(西北阿尔及利亚)供应盆地的干旱程度

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Meffrouche watershed, located in North-West Algeria with a land area of 89?km2, collects a mean annual rainfall of 659?mm (Meffrouche), computed over a period of 68 years (1943-1944 to 2010-2011). This basin, like most of the Maghreb, has been undergoing a persistent drought for a few decades. Different approaches, using a dataset of precipitation and depth of runoff, are addressed in this study to highlight the severity of this drought. The results obtained show the existence of a break of homogeneity located in the mid-1970s. The previous period is classified as wet, the one after is dry. The deficit between the two periods, valued at nearly 30?% for precipitation caused a drop in flow of more than 60?%. Periods of wetness and dryness are highlighted with a mild tendency to drought. Although some years have been very wet or extremely dry, the appearance of one or two years deficient rainfall in the mid-year surplus has no direct effect on water supplies in dam. For cons, the succession of several years with medium rainfall can generate a strong flow of water year.
机译:Meffrouche流域位于阿尔及利亚西北部,土地面积为89?km2,在68年的时间段(1943-1944年至2010-2011年)中,平均年降雨量为659?mm(Meffrouche)。与马格里布大部分地区一样,该盆地经历了数十年的持续干旱。本研究研究了使用降雨和径流深度数据集的不同方法,以突出说明这种干旱的严重性。获得的结果表明,在1970年代中期存在同质性断裂。前一个时期被分类为潮湿,第二个时期为干燥。两个时期之间的赤字约为30%,这是由于降水造成的赤字,导致流量下降了60%以上。潮湿和干燥的时期突出了轻度的干旱趋势。尽管有些年份非常潮湿或极度干燥,但在年中盈余中出现一到两年的降雨不足对大坝的供水没有直接影响。不利的是,连续几年降雨中等,可以产生大量的水。

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