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    Evaluation of decadal shoreline changes in the coastal region of Miri, Sarawak, Malaysia

    Access Status
    Fulltext not available
    Authors
    Anandkumar, A.
    Vijith, H.
    Ramasamy, Nagarajan
    Jonathan, M.P.
    Date
    2018
    Type
    Book Chapter
    
    Metadata
    Show full item record
    Citation
    Anandkumar, A. and Vijith, H. and Nagarajan, R. and Jonathan, M.P. 2019. Evaluation of Decadal Shoreline Changes in the Coastal Region of Miri, Sarawak, Malaysia, in Ramkumar, M. and James, A. and Menier, D. and Kumaraswamy, K. (eds), Coastal Zone Management, chapter 7, pp. 95-119. London, UK: Elsevier.
    Source Title
    Coastal Management: Global Challenges and Innovations
    DOI
    10.1016/B978-0-12-810473-6.00008-X
    ISBN
    9780128104750
    Faculty
    Curtin International
    School
    Curtin International
    URI
    http://hdl.handle.net/20.500.11937/79158
    Collection
    • Curtin Research Publications
    Abstract

    The coastal region of Miri City, Malaysia, in recent years has been excessively occupied by urbanization related to industrial development. The stress and changes in the climatic conditions in the region have induced changes in the shoreline over the last five decades. In this study, the landuse/landcover changes along with spatial and temporal characteristics of the shoreline have been studied for a 74 km coastal belt adjacent to Miri for a period covering 51 years, using geographical information systems (GIS). The landuse/landcover changes between the periods of 1968-2014 are identified and discussed in comparison with the spatial and temporal changes of shorelines in the study area. The results of the landuse/landcover change analysis have highlighted the massive conversion of primary forests as secondary forests, palm oil plantations, and urban areas over the last five decades. Shoreline change detection over the different time periods shows a decade of cyclic reversal of erosion and accretion along the shoreline of Miri. The major accretion spots and erosion hotspots are demarcated and the factors involved in this phenomenon are also identified. The increased sediment delivery through the rivers (the Baram, Miri, and Sibuti rivers) from the upper river catchment region and reclamation activities caused the accretion whereas the erosion hotspots are the results of unscientific development and coastal protection activities.

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