Kench Paul S
Department of Geography, National University of Singapore, Singapore; email:
Ann Rev Mar Sci. 2025 Jan;17(1):301-324. doi: 10.1146/annurev-marine-032223-030921. Epub 2024 Nov 25.
Coral reef islands are low-lying, wave-deposited sedimentary landforms. Using an eco-morphodynamic framework, this review examines the sensitivity of islands to climatic and environmental change. Reef island formation and morphological dynamics are directly controlled by nearshore wave processes and ecologically mediated sediment supply. The review highlights that reef islands are intrinsically dynamic landforms, able to adjust their morphology (size, shape, and location) on reef surfaces in response to changes in these processes. A suite of ecological and oceanographic processes also indirectly impact hydrodynamic and sediment processes and thereby regulate morphological change, though the temporal scales and magnitudes of impacts on islands vary, leading to divergent morphodynamic outcomes. Climatic change will modify the direct and indirect processes, causing complex positive and negative outcomes on islands. Understanding this complexity is critical to improve predictive capabilities for island physical change and resolve the timescales of change and lag times for impacts to be expressed in island systems.
珊瑚礁岛是地势低洼、由波浪沉积形成的地貌。本综述采用生态地貌动力学框架,研究了这些岛屿对气候和环境变化的敏感性。礁岛的形成和形态动力学直接受近岸波浪过程和生态介导的沉积物供应控制。该综述强调,礁岛本质上是动态地貌,能够根据这些过程的变化在礁表面调整其形态(大小、形状和位置)。一系列生态和海洋学过程也间接影响水动力和沉积过程,从而调节形态变化,尽管对岛屿影响的时间尺度和幅度各不相同,导致不同的地貌动力学结果。气候变化将改变直接和间接过程,给岛屿带来复杂的正负结果。理解这种复杂性对于提高对岛屿物理变化的预测能力、确定变化的时间尺度以及影响在岛屿系统中显现的滞后时间至关重要。