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Assessing multi-decadal shoreline change and future sea level projections to support coastal adaptation in Selangor, Malaysia

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Coastal zones worldwide face escalating pressures from climate change and urbanization, yet the geomorphological stability of tropical coastlines remains a critical research gap. This study assesses multi-decadal shoreline change along a 250 km corridor of Selangor, Malaysia, utilizing Landsat data and the Digital Shoreline Analysis System. Results reveal localized erosion hotspots and project intensifying erosive trends by 2050, informing climate adaptation strategies. For deeper insights into integrating climate data into environmental impact assessments, see our related article, "From climate data to regulatory decisions."
Assessing multi-decadal shoreline change and future sea level projections to support coastal adaptation in Selangor, Malaysia

The accelerating impacts of climate change on coastal regions demand rigorous, data-driven assessments to inform effective adaptation strategies. A recent study evaluating shoreline dynamics along the Selangor coastline in Malaysia underscores this necessity, highlighting the complex interplay of natural processes and human influence. The research, utilizing a longitudinal analysis of Landsat imagery spanning three decades and employing the Digital Shoreline Analysis System (DSAS), provides a valuable baseline understanding of geomorphological stability in a critical tropical, mud-dominated environment. This work builds on the growing body of research attempting to translate climate data into actionable insights, as explored in articles such as From climate data to regulatory decisions: integrating climate AI into marine EIAs, which examines the integration of climate AI into marine Environmental Impact Assessments. The study's focus on a 250km stretch of coastline, combined with the application of the Geomorphological Stability Index (GSI), allows for a nuanced understanding of localized erosion hotspots and broader trends, a level of detail vital for targeted interventions. The observed discrepancies between End Point Rate (EPR) and Linear Regression Rate (LRR) metrics further emphasize the importance of employing multiple analytical approaches to capture the dynamic nature of coastal change.

The findings reveal a concerning picture: severe erosion hotspots, particularly near the Port Klang complex, and a projection of intensifying erosive trends by 2050. The GSI classification, indicating a significant portion of the shoreline as either highly stable/accreting or severely eroding, underscores the heterogeneity of coastal response. The study’s high framework sensitivity, validated against an independent hazard inventory, further strengthens the reliability of its projections. These projections align with broader concerns regarding the vulnerability of coastal ecosystems and human populations to climate change, a theme also addressed in Sandy littorals under threat: a comprehensive review of the impacts of climate change on plant-dominated components relevant to the Mediterranean littoral active zone, which highlights the impacts on plant-dominated coastal components. The Selangor study’s contribution lies in the spatially explicit, scenario-based projections that can directly inform coastal adaptation strategies. The use of IPCC AR6 sea level rise anomalies demonstrates a commitment to using the most current and validated climate data available, a crucial element for creating robust and reliable projections.

Beyond the immediate implications for Selangor, Malaysia, this research offers a methodological framework applicable to other mud-dominated tropical coastlines facing similar challenges. The integration of historical data, advanced geospatial techniques, and climate projections provides a robust approach to assessing coastal vulnerability and guiding adaptation planning. The development of the GSI, in particular, represents a valuable tool for coastal managers seeking to prioritize interventions and allocate resources effectively. The study also implicitly reinforces the importance of understanding the complex interactions between natural processes and anthropogenic activities – the engineered Port Klang complex clearly demonstrates how human infrastructure can exacerbate coastal erosion. Further research should focus on refining the GSI to incorporate additional variables, such as sediment transport dynamics and the impact of extreme weather events, to enhance its predictive capabilities. The calibration of these models, as discussed in Research on China’s green total factor productivity of aquaculture industry and its influencing factors, requires ongoing empirical validation and refinement.

Ultimately, this study exemplifies the critical role of ocean intelligence—integrated data ecosystems providing real-time and validated information—in supporting informed decision-making regarding coastal resilience. The actionable screening data generated by this research represents a significant step towards proactive adaptation in the face of accelerating climate change. As sea levels continue to rise and storm intensity increases, the ability to accurately predict and mitigate coastal erosion will be paramount. A crucial question moving forward is how these localized, high-resolution assessments can be scaled and integrated into national and regional coastal management frameworks to ensure equitable and effective adaptation across vulnerable communities.

Coastal zones are increasingly exposed to climate change and rapid urbanization, yet the geomorphological stability of tropical, mud-dominated coastlines remains poorly understood. This study evaluates multi-decadal shoreline dynamics along a 250 km corridor of the Selangor coastline, Peninsular Malaysia, from 1990 to 2020. Using seven multi-temporal, sensor-homogenized Landsat datasets, baseline change metrics were computed via the Digital Shoreline Analysis System (DSAS v5.1). Historical shoreline shifts were quantified using the End Point Rate (EPR) and Linear Regression Rate (LRR) metrics to construct a process-based Geomorphological Stability Index (GSI). These historical vectors were coupled with IPCC AR6 sea-level rise anomalies to simulate scenario-based exposure projections for the 2030, 2040, and 2050 horizons. Baseline results revealed severe localized erosion hotspots exceeding -75 m/yr near the highly engineered Port Klang complex. The EPR network yielded a net erosional tendency of -0.15 m/yr, whereas the LRR model revealed a marginal net accretionary trend of +0.30 m/yr. The GSI framework classified 53.19% of the transects as highly stable/accreting (Rank 5) and 32.92% as severely eroding (Rank 1). Validation against an independent hazard inventory demonstrated a framework sensitivity of 100.0%. Scenario-based projections reveal intensifying erosive trends by 2050, accelerating mean EPR erosion to -5.14 m/yr and destabilizing up to 49% of the shoreline footprint. The findings provide actionable screening data to guide climate adaptation strategies.

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