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Satellite-derived changes in floodplain productivity and freshwater habitats in northern Australia (1991-2019)

机译:澳大利亚北部洪泛区生产力和淡水栖息地的卫星改变(1991-2019)

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摘要

The ecological communities supported by freshwater habitats and wetlands that persist from floodplain inundation generate numerous cultural, recreational and economic values via commercial fisheries and other human uses of these habitats. However, the alteration of flow connectivity, degradation, and disruption of physical processes that sustain different levels of organisms (e.g., primary producers) are threats that affect aquatic biodiversity and the productivity of these habitats. Therefore, the large scale assessment of freshwater habitats for proactive water resources planning and the development of climate change mitigation and resource management strategies is essential. However, such monitoring and assessment is complicated by the inaccessibility of many large wetland systems during times of inundation, making in situ sampling unfeasible at a time when high levels of aquatic primary producers are generating food and energy sources for higher order consumers. To understand the physical dynamics of aquatic primary producers and freshwater habitats (1991-2019) during such times in a large floodplain river in northern Australia (Gilbert catchment), this study integrated Landsat-derived modified normalised difference water index and normalised difference vegetation index in a classification tree model. Thereafter, key hydrological drivers (rainfall and river discharge) of floodplain productivity and connectivity were assessed using a range of multivariate techniques. Results show that the floodplain had a high aquatic plant biomass during the summer wet season based on the correlation between aquatic biomass accumulation (hot spots) and inundation (r = 0.83 @ phase lag 1 month) during such period. River discharge (r = 0.68 @ lag = 1 month) at downstream Gilbert catchment appear to be a relatively stronger indicator of hot spots of floodplain biomass accumulation as opposed to local rainfall (r = 0.57 @ lag = 3 months). While the downstream discharge explains a significant proportion of variability in the leading orthogonal mode of rainfall (r = 0.83), statistical relationships developed between discharge/rainfall and the distribution of aquatic primary producers confirm that both rivers (flow) and local rainfall are key optimal predictors of inundation and sites of primary producers with river flows being a better indicator of the latter. It is therefore argued that hydro-meteorological fluctuations will be key constraints on freshwater habitats and the growth of primary producers, albeit, human disturbance of flow can impact on floodplain productivity. As illustrated in this study, such constraints are reflected in the spatial patterns and changing characteristics (connectivity and spatial heterogeneity) of hot spots of primary producers and freshwater habitats (Palustrine, Lacustrine, and Riverine ecosystems).
机译:淡水栖息地和湿地支持的生态社区通过洪泛区淹没,通过商业渔业和这些栖息地的其他人类用途产生了许多文化,娱乐和经济价值。然而,在维持不同生物水平(例如,主要生产商)的流动连接,降解和破坏物理过程中断的改变是影响水生生物多样性和这些栖息地生产力的威胁。因此,对积极水资源规划的淡水栖息地的大规模评估和气候变化的发展缓解和资源管理策略至关重要。然而,这种监测和评估是由于许多大型湿地系统在淹没期间的不可行,在高水平的水生生产者正在为高阶消费者产生食物和能源时,原位取样是不可行的。在澳大利亚北部大型洪泛河(Gilbert Condrammer)的大型洪泛河(Gilbert Condramment)中,了解水生初级生产者和淡水栖息地(1991-2019)的物理动态,这项研究综合兰德拉斯衍生的修改归一化差异水指数和归一化差异植被指数分类树模型。此后,使用一系列多变量技术评估泛洪叶生产率和连接的关键水文驱动器(降雨和河流排放)。结果表明,基于在此期间的水生生物量积累(热点)和淹没(r = 0.83×1个月)之间的相关性,洪泛区在夏季潮汐季节进行了高水生植物生物量。下游吉尔伯特集水区的河流放电(r = 0.68 @ lag = 1个月)似乎是洪泛区生物质积累的热点指标,而不是当地降雨(r = 0.57 @ lag = 3个月)。虽然下游放电解释了在暴雨中的主要正交模式下的显着比例(R = 0.83),但排放/降雨与水生主要生产商的分布之间产生的统计关系确认河流(流量)和局部降雨是关键的最佳选择河流流量的淹没和田间境外的预测因素是后者的更好指标。因此,有人认为水流波动将是对淡水栖息地的关键限制以及初级生产者的生长,尽管的流动障碍可能会影响洪泛平原生产力。如本研究中所示,这种约束反映在主要生产商和淡水栖息地(Palustrine,Lapustine和河流生态系统)的热点的空间模式和变化特性(连接和空间异质性)。

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