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Thresholds of sea‐level rise rate and sea‐level rise acceleration rate in a vulnerable coastal wetland

机译:脆弱的沿海湿地海平面上升速度和海平面上升加速的阈值

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摘要

Feedbacks among inundation, sediment trapping, and vegetation productivity help maintain coastal wetlands facing sea‐level rise (SLR). However, when the SLR rate exceeds a threshold, coastal wetlands can collapse. Understanding the threshold helps address key challenges in ecology—nonlinear response of ecosystems to environmental change, promotes communication between ecologists and resource managers, and facilitates decision‐making in climate change policies. We studied the threshold of SLR rate and developed a new threshold of SLR acceleration rate on sustainability of coastal wetlands as SLR is likely to accelerate due to enhanced anthropogenic forces. Deriving these two thresholds depends on the temporal scale, the interaction of SLR with other environmental factors, and landscape metrics, which have not been fully accounted for before this study. We chose a representative marine‐dominated estuary in the northern Gulf of Mexico, Grand Bay in Mississippi, to test the concept of SLR thresholds. We developed a mechanistic model to simulate wetland change and then derived the SLR thresholds for Grand Bay. The model results show that the threshold of SLR rate in Grand Bay is 11.9 mm/year for 2050, and it drops to 8.4 mm/year for 2100 using total wetland area as a landscape metric. The corresponding SLR acceleration rate thresholds are 3.02 × 10−4 m/year2 and 9.62 × 10−5 m/year2 for 2050 and 2100, respectively. The newly developed SLR acceleration rate threshold can help quantify the temporal lag before the rapid decline in wetland area becomes evident after the SLR rate threshold is exceeded, and cumulative SLR a wetland can adapt to under the SLR acceleration scenarios. Based on the thresholds, SLR that will adversely impact the coastal wetlands in Grand Bay by 2100 will fall within the likely range of SLR under a high warming scenario ( style="fixed-case">RCP8.5), highlighting the need to avoid style="fixed-case">RCP8.5 to preserve these marshes.
机译:淹没,沉积物捕集和植被生产力之间的反馈有助于维持沿海湿地面临海平面上升(SLR)。但是,当SLR率超过阈值时,沿海湿地可能崩溃。了解阈值有助于解决生态系统中的关键挑战,即生态系统对环境变化的非线性响应,促进生态学家和资源管理者之间的沟通,并促进气候变化政策的决策。我们研究了SLR率的阈值,并为沿海湿地的可持续性开发了新的SLR加速度率阈值,因为人为力量增强可能会使SLR加速。推导这两个阈值取决于时间尺度,SLR与其他环境因素的相互作用以及景观指标,在此研究之前尚未完全考虑。我们选择了在墨西哥湾北部,密西西比州的格兰德湾具有代表性的海洋主导性河口,以测试SLR阈值的概念。我们开发了一个机械模型来模拟湿地变化,然后得出了格兰德湾的SLR阈值。模型结果表明,以湿地总面积为景观度量标准,到2050年,格兰德湾的SLR率阈值为11.9毫米/年,而对于2100年,其下降至8.4毫米/年。相应的SLR加速度阈值是3.02×10 −4 m / year 2 和9.62×10 -5 m / year 2 分别表示2050和2100。新开发的SLR加速速率阈值可以帮助量化在超过SLR速率阈值后湿地面积的迅速下降变得明显之前的时间滞后,并且湿地的累积SLR可以适应SLR加速场景。根据这些阈值,到2100年将对大湾沿岸湿地产生不利影响的SLR将在高变暖情况下( style =“ fixed-case”> RCP 8.5)落在SLR的可能范围内,强调需要避免 style =“ fixed-case”> RCP 8.5保留这些沼泽。

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