Abstract

The Maldives, with one of the lowest average land elevations above present-day mean sea level, is among the world regions that will be the most impacted by mean sea-level rise and marine extreme events induced by climate change. Yet, the lack of regional and local information on marine drivers is a major drawback that coastal decision-makers face to anticipate the impacts of climate change along the Maldivian coastlines. In this study we focus on wind-waves, the main driver of extremes causing coastal flooding in the region. We dynamically downscale large-scale fields from global wave models, providing a valuable source of climate information along the coastlines with spatial resolution down to 500 m. This dataset serves to characterise the wave climate around the Maldives, with applications in regional development and land reclamation, and is also an essential input for local flood hazard modelling. We illustrate this with a case study of HA Hoarafushi, an atoll island where local topo-bathymetry is available. This island is exposed to the highest incoming waves in the archipelago and recently saw development of an airport island on its reef via land reclamation. Regional waves are propagated toward the shoreline using a phase-resolving model and coastal inundation is simulated under different mean sea-level rise conditions of up to 1 m above present-day mean sea level. The results are represented as risk maps with different hazard levels gathering inundation depth and speed, providing a clear evidence of the impacts of the sea level rise combined with extreme wave events.

Highlights

  • Increased coastal flooding damages are among the potentially most hazardous and costliest aspects of global warming (Hinkel et al, 2014), impacting populations, ecosystems and assets

  • Our findings indicate that a moderate incoming southwestern swell corresponding to a return period of only 10 years will cause overtopping in Hoarafushi island if it reaches the shoreline under a mean sea level 0.75 m higher than its present-day value (Figure 9)

  • Our study provides the framework to fill the gap between global information of marine climate drivers, including mean sea level and extremes, and local coastal flood hazard modelling

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Summary

INTRODUCTION

Increased coastal flooding damages are among the potentially most hazardous and costliest aspects of global warming (Hinkel et al, 2014), impacting populations, ecosystems and assets. In 2007, the Fares island, located in the southernmost atoll of the Maldives was flooded due to a series of remotely-generated swell events reaching the island (Wadey et al, 2017; Beetham and Kench, 2018) which affected other areas of the eastern Indian Ocean (e.g., Lecacheux et al, 2012 in La Réunion Island). This event was hazardous as it flooded almost the entire island and affected more than 1500 people as well as the limited water resources of the island.

DATA AND METHODS
Global Wind-Wave Datasets
Regional Wave Modelling
Local Wave Modelling
Present-Day Wave Climate
Wave Projections During the Twenty-First Century
REGIONAL WAVE DOWNSCALING
LOCAL WAVE MODELLING AND FLOOD HAZARD IN HOARAFUSHI ISLAND
Global to Local Coastal Modelling
Application for Coastal Flood Hazard
CONCLUDING REMARKS
Findings
DATA AVAILABILITY STATEMENT
Full Text
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