The Vietnamese Mekong Delta (VMD) is one of the world’s most vulnerable deltas to climate change
and sea level rise. Adequate understandings of future hydrological changes are crucial for effective
water management and risk-proofing, however, this knowledge body is currently very limited. This
study quantifies the responses of the VMD’s river flow regime to multiple stimuli, namely future
upstream inflow variation, local climate change, and sea level rise. The one-dimensional
hydrodynamic model MIKE 11 was used to simulate discharges and water levels across the delta.
We developed four scenarios to represent changes in the upstream discharges, precipitation
changes and sea level rise, covering the 2036–2065 period. We downscaled climate data and
applied three bias-correction methods for five General Circulation Models (GCM), and two
Representative Concentration Pathways (RCPs). The climate change projections show similar trends
of increasing wet season precipitation and decreasing dry season precipitation. However, crossscenario
variations are sometimes large, depending on the individual GCMs, the RCPs and specific
locations. The hydraulic simulation results indicate that, under discharge changes between −20%
and +10%, combined with in-delta precipitation variations during the dry season, river discharges
at the four representative stations could reduce substantially from −2.5% to −100.2%. During the
wet season, the calculated river discharges show increase between 7.3% and 46.7% under four
considered scenarios. Substantial changes in the VMD’s river flow regime could have potentially
serious implications for water management, especially saltwater intrusion, and therefore calling for
timely adaptation measures.
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The Vietnamese Mekong Delta (VMD) is one of the world’s most vulnerable deltas to climate change
and sea level rise. Adequate understandings of future hydrological changes are crucial for effective
water management and risk-proofing, however, this knowledge body is currently very limited. This
study quantifies the responses of the VMD’s river flow regime to multiple stimuli, namely future
upstream inflow variation, local climate change, and sea level rise. The one-dimensional
hydrodynamic m...
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