Abstract

The Pacific region consists of numerous Small Island Developing States (SIDS), one of the most vulnerable to flooding caused by compound effects of sea level rise (SLR) and storms. Nevertheless, individual studies regarding the impact assessment for SIDS, such as the low-lying Kiribati, remain scarce. This study assessed the impact of climate change-induced storm surge and SLR compounding effects on Tarawa, the most populous atoll of Kiribati, the largest coral atoll nation. It projected the impact using a combined dynamic surge and SLR model based on the IPCC AR5 RCP scenarios and 1/100 and 1/50 years return period storm events. This approach allows estimating the inundation scope and the consecutive exposed population by the end of the 21st century. The results of this study show that the pace of SLR is pivotal for Tarawa, as the sea level rise alone can claim more than 50% of the territory and pose a threat to over 60% of the population under the most intense greenhouse gas emissions scenario. Furthermore, most coasts on the lagoon side are particularly vulnerable. In contrast, the contribution of extreme events is generally minimal due to low wind speeds and the absence of tropical cyclones (TC). Despite this, it is clear the compound effects are critical and may inescapably bring drastic changes to the atoll nations by the end of this century. The impact assessment in this study draws attention to the social impact of climate change on SIDS, most notably atoll islands, and evaluates their adaptation potential.

Highlights

  • This study focuses on Tarawa Atoll (Kiribati), a low-lying atoll island located in Oceania

  • According to the RCP2.6 scenario, the sea level rise (SLR) alone will cause inundation of 4.58 km2, or 14.76% of the total land area, while the RCP8.5 estimated that the inundation area will be 2.5 times larger, i.e., 11.47 km2 of the total land area

  • Betio area located on the western tip is susceptible to severe inundation even in the RCP2.6 scenario in the future

Read more

Summary

Introduction

One of the phenomena directly related to climate change is sea level rise (SLR). The SLR is the average long-term rise of the ocean surface globally, as observed by the coastal tide gauge and satellite data. According to NASA’s satellite sea level observations, the sea height variation has increased by 99 (±4) mm between January 1993 and May 2021, making a rate of change 3.4 mm/ year globally (NASA’s Goddard Space Flight Center, 2021). This number is more than two times

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call