Evolution of river regimes in the Mekong River basin over 8 decades and the role of dams in recent hydrological extremes

Huy Dang, Y. Pokhrel
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Abstract

Abstract. Flow regimes in major global river systems are undergoing rapid alterations due to unprecedented stress from climate change and human activities. The Mekong River basin (MRB) was, until recently, among the last major global rivers relatively unaltered by humans, but this has been changing alarmingly in the last decade due to booming dam construction. Numerous studies have examined the MRB's flood pulse and its alterations in recent years. However, a mechanistic quantification at the basin scale attributing these changes to either climatic or human drivers is lacking. Here, we present the first results of the basin-wide changes in natural hydrological regimes in the MRB over the past 8 decades and the impacts of dams in recent decades by examining 83 years (1940–2022) of river regime characteristics simulated by a river–floodplain hydrodynamic model that includes 126 major dams in the MRB. Results indicate that, while the Mekong River's flow has shown substantial decadal trends and variabilities, the operation of dams in recent years has been causing a fundamental shift in the seasonal volume and timing of river flow and extreme hydrological conditions. Even though the dam-induced impacts have been small so far and most pronounced in areas directly downstream of major dams, dams are intensifying the natural variations in the Mekong's mainstream wet-season flow. Further, the additional 65 dams commissioned since 2010 have exacerbated drought conditions by substantially delaying the MRB's wet-season onset, especially in recent years (e.g., 2019 and 2020), when the natural wet-season durations are already shorter than in normal years. Further, dams have shifted by up to 20 % of the mainstream annual volume between the dry and wet seasons in recent years. While this has a minimal impact on the MRB's annual flow volume, the flood occurrence in many major areas of Tonlé Sap and the Mekong Delta has been largely altered. This study provides critical insights into the long-term hydrological variabilities and impacts of dams on the Mekong River's flow regimes, which can help improve water resource management in light of intensifying hydrological extremes.
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湄公河流域八十年来河流水系的演变以及大坝在近期极端水文现象中的作用
摘要由于气候变化和人类活动造成的前所未有的压力,全球主要河流系统的水流状态正在发生迅速变化。直到最近,湄公河流域(MRB)仍是全球最后几条相对未受人类影响的主要河流之一,但在过去十年中,由于大坝建设的蓬勃发展,这种情况正在发生令人震惊的变化。近年来,许多研究都对 MRB 的洪水脉冲及其变化进行了研究。然而,目前还缺乏在流域尺度上将这些变化归因于气候或人类驱动因素的机理量化研究。在此,我们通过研究包括湄公河流域 126 座主要大坝在内的河流-洪泛平原水动力模型模拟的 83 年(1940-2022 年)河流水文特征,首次展示了过去 80 年来湄公河流域全流域自然水文机制的变化以及近几十年来大坝的影响。研究结果表明,虽然湄公河的水流呈现出显著的十年趋势和变化,但近年来大坝的运行已导致河水的季节性流量和时间以及极端水文条件发生了根本性的变化。尽管到目前为止,大坝造成的影响还很小,而且在主要大坝的直接下游地区最为明显,但大坝正在加剧湄公河主流雨季流量的自然变化。此外,自 2010 年以来,又有 65 座大坝投入使用,大大推迟了湄公河干流雨季的开始时间,从而加剧了干旱状况,尤其是在近几年(如 2019 年和 2020 年),自然雨季的持续时间已经短于正常年份。此外,近年来,大坝在旱季和雨季之间转移了多达 20% 的主流年水量。虽然这对湄公河干流的年流量影响很小,但洞里萨湖和湄公河三角洲许多主要地区的洪水发生率却发生了很大变化。这项研究提供了关于长期水文变化和大坝对湄公河流量机制影响的重要见解,有助于在极端水文现象加剧的情况下改善水资源管理。
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