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Changes in the areal extents of the Athabasca River, Birch River, and Cree Creek Deltas, 1950-2014, Peace-Athabasca Delta, Canada

机译:加拿大阿萨巴斯卡三角洲和平地区,阿萨巴斯卡河,桦木河和克里溪三角洲面积变化,1950-2014年

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Deltas form where riverborne sediment accumulates at the interface of river mouths and their receiving water bodies. Their areal extent is determined by the net effect of processes that increase their extent, such as sediment accumulation, and processes that decrease their extent, such as erosion and subsidence. Through sequential mapping and construction of river discharge and sediment histories, this study examined changes in the subaerial extents of the Cree Creek and Athabasca River Deltas (both on the Athabasca River system) and the Birch River Delta in northern Canada over the period 1950-2014. The purpose of the study was to determine how, when, and why the deltas changed in areal extent. Temporal growth patterns were similar across the Athabasca and Birch River systems indicative of a climatic signal. Little or no areal growth occurred from 1950 to 1968; moderate growth occurred between 1968 and the early to mid-1980s; and rapid growth occurred between 1992 and 2012. Factors that affected delta progradation included dredging, sediment supply, isostatic drowning, delta front bathymetry, sediment capture efficiency, and storms. In relation to sediment delivered, areal growth rates were lowest in the Athabasca Delta, intermediate in the Birch Delta, and highest in the Cree Creek Delta. Annual sediment delivery is increasing in the Cree Creek Delta; there were no significant trends in annual sediment delivery in the Birch and Athabasca Deltas. There was a lag of up to several years between sediment delivery events and progradation. Periods of delta progradation were associated with low water levels of the receiving basins. Predicted climate-change driven declines in river discharge and lake levels may accelerate delta progradation in the region. In the changing ecosystems of northeastern Alberta, inadequate monitoring of vegetation, landforms, and sediment regimes hampers the elucidation of the nature, rate, and causality of ecosystem changes. (C) 2016 Elsevier B.V. All rights reserved.
机译:三角洲的形成是河床沉积物在河口及其接收水体的界面处积聚。其面积范围由增加其范围的过程(如沉积物堆积)和减少其范围的过程(如侵蚀和沉降)的净效应决定。通过顺序绘制地图以及河流流量和泥沙历史的构建,本研究研究了1950-2014年间Cree Creek和Athabasca河三角洲(均在Athabasca河系上)和加拿大北部的Birch河三角洲的陆上变化。该研究的目的是确定三角洲面积变化的方式,时间和原因。阿萨巴斯卡和伯奇河水系的时间增长模式相似,表明气候信号。从1950年到1968年,几乎没有或根本没有面积增长。在1968年至1980年代初至中期之间出现适度增长;在1992年至2012年之间出现了快速增长。影响三角洲发育的因素包括疏ging,沉积物供应,等静压溺水,三角洲前测深,沉积物捕获效率和暴风雨。关于沉积物的输送,阿萨巴斯卡三角洲的面积增长率最低,桦木三角洲的中等,克里河溪三角洲的最高。在克里溪三角洲,每年的泥沙输送量正在增加。在桦木和阿萨巴斯卡三角洲地区,每年的泥沙输送量没有明显的趋势。沉积物输送事件和水结过程之间存在长达数年的滞后。三角洲发育时期与接收盆地的低水位有关。预测的气候变化驱动的河流流量和湖泊水位下降可能会加速该地区的三角洲发展。在阿尔伯塔省东北部不断变化的生态系统中,对植被,地貌和沉积物制度的监测不足,难以阐明生态系统变化的性质,速度和因果关系。 (C)2016 Elsevier B.V.保留所有权利。

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