河流调控和气候变化对摩洛哥南部Oued Massa河口的影响

H. Fox, R. Wilby, H. Moore
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引用次数: 21

摘要

摩洛哥南部的Oued Massa河口经历了潮汐和泻湖条件的交替阶段。利用野外调查、航空摄影和降雨径流记录,描述了河口的主要过程和最近的演变。这些数据表明,自上游被Youssef Ben Tachfine水库截流以来,河口的特征发生了变化。由于河流整治,低流量的频率显著增加,洪水事件之间的平均间隔时间也显著增加。利用重建的流量序列推测,在蓄水后的时代,泻湖条件比20世纪20年代以来的任何时候都更为普遍。尽管全球气候模式HadCM2预测的2030-2049年冬季降水增加意味着未来洪水进入水库的频率更高,但这种流入的幅度和频率仍在历史变率范围内。尽管如此,较高的流入可能会导致更频繁的溢出,并伴随着沙洲的破裂和泻湖阶段的终止。尽管如此,有人认为大坝的存在最终会对河口-泻湖系统的功能产生比该地区未来降水变化更大的影响。版权所有©2001约翰威利父子有限公司
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The impact of river regulation and climate change on the barred estuary of the Oued Massa, southern Morocco
The estuary of the Oued Massa, southern Morocco, has experienced alternating phases of tidal and lagoon conditions. Using field surveys, aerial photographs and rainfall–runoff records the dominant processes and recent evolution of the estuary are described. These data suggest that the character of the estuary has changed since the upstream impoundment of the river by the Youssef Ben Tachfine reservoir. The frequency of low-flows has been significantly increased by river regulation, as has the mean interval between flood events. Using reconstructed flow series it is speculated that lagoon conditions have become more common in the post-impoundment era than at any time since the 1920s. Although increases in winter precipitation projected by the global climate model HadCM2 for 2030–2049 imply a higher frequency of flood flows entering the reservoir in the future, the magnitude and frequency of such inflows are still within historic variability. Nonetheless, higher inflows may produce more frequent spills with concomitant bar breaching and termination of lagoon phases. Despite this, it is argued that the presence of the dam is ultimately of greater consequence to the functioning of the estuary–lagoon system than future precipitation changes over the region. Copyright © 2001 John Wiley & Sons, Ltd.
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