GeoQuEST Research Centre, School of Earth and Environmental Sciences, University of Wollongong, Wollongong, 2522, Australia.
Department of Geography, University of Babylon, Ministry of Higher Education and Scientific Research, Hillah, Iraq.
Environ Monit Assess. 2018 Jun 3;190(7):375. doi: 10.1007/s10661-018-6720-5.
Monitoring estuarine ecological-geomorphological dynamics has become a crucial aspect of studying the impacts of climate change and worldwide infrastructure development in coastal zones. Together, these factors have changed the natural eco-geomorphic processes that affect estuarine regimes and comprehensive modelling of coastal resources can assist managers to make appropriate decisions about their sustainable use. This study has utilised Towamba estuary (southeastern NSW, Australia), to demonstrate the value and priority of modelling estuarine dynamism as a measure of the rates and consequences of eco-geomorphic changes. This research employs several geoinformatic modelling approaches over time to investigate and assess how climate change and human activities have altered this estuarine eco-geomorphic setting. Multitemporal trend/change analysis of sediment delivery, shoreline positions and land cover, determined from fieldwork and GIS analysis of remote sensing datasets, shows significant spatio-temporal changes to the elevation and areal extent of sedimentary facies in the Towamba estuary over the past 65 years. Geomorphic growth (~ 2600 m annually) has stabilised the estuarine habitats, particularly within native vegetation, salt marsh and mangrove areas. Geomorphic changes have occurred because of a combination of sediment runoff from the mostly unmodified terrestrial catchment, nearshore processes (ocean dynamics) and human activities. The construction of GIS models, verified with water and sediment samples, can characterise physical processes and quantify changes within the estuarine ecosystem. Such robust models will allow resource managers to evaluate the potential effects of changes to the current coastal ecosystems.
监测河口生态地貌动态已成为研究气候变化和全球沿海基础设施发展对沿海地区影响的关键方面。这些因素共同改变了影响河口状态的自然生态地貌过程,对沿海资源进行综合建模可以帮助管理者就其可持续利用做出适当决策。本研究利用托旺巴河口(澳大利亚新南威尔士州东南部),展示了对河口动力进行建模的价值和优先级,以此作为衡量生态地貌变化速率和后果的一种手段。本研究采用了多种地理信息建模方法,随着时间的推移来研究和评估气候变化和人类活动如何改变了这个河口的生态地貌环境。通过对遥感数据集的野外工作和 GIS 分析,对泥沙输送、海岸线位置和土地覆盖的多时相趋势/变化分析表明,在过去 65 年中,托旺巴河口的沉积相高程和面积范围发生了显著的时空变化。地貌生长(每年约 2600 米)稳定了河口栖息地,特别是在本地植被、盐沼和红树林地区。地貌变化是由于来自大部分未经改造的陆地流域的泥沙径流、近岸过程(海洋动力)和人类活动的综合作用造成的。通过与水和泥沙样本进行验证的 GIS 模型的构建,可以描述物理过程并量化河口生态系统内的变化。这种强大的模型将使资源管理者能够评估当前沿海生态系统变化的潜在影响。