海岸带复杂系统的协同演化与驱动机制Co-evolution and driving mechanisms of complex coastal systems
人类活动和气候变化首先改变海岸线物理结构,随后影响 C/N/P 迁移转化和生态系统功能。岸线硬化、围填海、港口开发和流域输入改变水动力边界、沉积物交换和营养盐滞留;海温升高、酸化、脱氧和海平面上升进一步放大通量压力,推动栖息地连通性、生物群落和生态系统功能重组Human activity and climate change first alter the physical structure of shorelines and then reshape C/N/P transport, transformation, and ecosystem function. Shoreline hardening, reclamation, port development, and watershed inputs change hydrodynamic boundaries, sediment exchange, and nutrient retention; warming, acidification, deoxygenation, and sea-level rise further amplify flux pressure and reorganize habitat connectivity, biological communities, and ecosystem functions.
变量体系覆盖岸线位置与类型、潮滩湿地面积、悬沙与沉积速率、河口营养盐负荷、近岸碳通量、溶解氧、叶绿素、pH、生物多样性、土地利用和社会经济压力。多源遥感、现场观测、沉积档案、历史统计、区域模拟和跨模态数据融合建立可对比的长期序列The variable system covers shoreline position and type, tidal-flat wetland area, suspended sediment and sedimentation rates, estuarine nutrient loads, coastal carbon fluxes, dissolved oxygen, chlorophyll, pH, biodiversity, land use, and socioeconomic pressure. Multi-source remote sensing, field observations, sediment archives, historical statistics, regional simulation, and cross-modal data fusion build comparable long-term sequences.