Abstract

Water infrastructure development is crucial for driving economic growth in the developing countries of the Mekong. Yet it may also alter existing hydrological and flood conditions, with serious implications for water management, agricultural production and ecosystem services, especially in the floodplain regions. Our current understanding of the hydrological and flood pattern changes associated with infrastructural development still contain several knowledge gaps, such as the consideration of overlooked prospective drivers, and the interactions between multiple drivers. This research attempts to conduct a cumulative impact assessment of flood changes in the Cambodian part of the Mekong floodplains. The developmental activity of six central sectors (hydropower, irrigation, navigation, flood protection, agricultural land use and water use) as well as climate change were considered in our modelling analysis. Our results show that the monthly, sub-seasonal, and seasonal hydrological regimes will be subject to substantial alterations under the 2020 planned development scenario, and even larger alterations under the 2040 planned development scenario. The degree of hydrological alteration under the 2040 planned development is somewhat counteracted by the effect of climate change, as well as the removal of mainstream dams in the Lower Mekong Basin and hydropower mitigation investments. The likely impact of decreasing water discharge in the early wet season (up to −34 %) will pose a critical challenge to rice production, whereas the likely increase in water discharge in the mid-dry season (up to +54 %) indicates improved water availability for coping with drought stresses and sustaining environmental flow. At the same time, these changes would have drastic impacts on total flood extent, which is projected to decline up to −18 %, having potentially negative impacts on floodplain productivity whilst at the same time reducing the flood risk to the area. Our findings urge the timely establishment of adaptation and mitigation strategies to manage such future environmental alterations in a sustainable manner.

Highlights

  • The Mekong River Basin (MRB) is the largest river basin in the Southeast Asian mainland

  • Based on the validation measures (Table 3), a good model performance is obtained at all stations with the values of Nash-Sutcliffe efficiency (NSE) between 0.62 and 0.96, percent bias (PBIAS) between –3.68% and +20.66%, RSR between 0.19 and

  • It is apparent that the simulated water discharge 200 among these stations is well in line with the observed data throughout the 24-year study period; three stations, namely Kampong Cham, Chruy Changvar, and Neak Loeung overestimate the peak water discharge and water level

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Summary

Introduction

The Mekong River Basin (MRB) is the largest river basin in the Southeast Asian mainland. Cyclones and severe tropical storms have generated the most significant Mekong flooding events, the largest of which was recorded in 1966, when tropical storm Phyllis struck the Upper Mekong Basin (UMB) (Adamson et al, 2009). Discussion started: 12 March 2021 c Author(s) 2021. Confluence of the Mekong River, and within the Mekong Delta. The last severe flood occurred in 2011 and it is ranked among the highest discharge recorded in the Lower Mekong Basin (LMB) (MRC, 2011)

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