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Palaeohydrology in climatological context: Developing the case for use of remote predictors in Australian streamflow reconstructions

机译:气候背景下的古水文:为在澳大利亚河流重建中使用远程预报器的案例开发

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The dry continent of Australia experiences frequent periods of devastating regional drought, making high quality palaeohydrological reconstructions essential for water resource management and planning. In other parts of the world tree-rings form a core component of such reconstructions. Yet for much of Australia, annually resolved palaeohydrological reconstructions derived from tree-rings have proven elusive. The island state of Tasmania in the far south is an important exception, with over 50 tree-ring chronologies available. Coupled ocean-atmosphere processes that drive precipitation across mainland Australia also influence Tasmanian precipitation. Here, we provide a basic analysis of how geographic relationships between important drivers of seasonal Tasmanian streamflow and potential streamflow predictors such as tree-ring chronologies may extend the spatial applicability of Tasmania's tree-ring predictors beyond the local context. We find clear geographically and seasonally defined patterns in Tasmanian streamflow that are reflected in the relationships between individual Tasmanian tree-ring chronologies and their relationships with streamflows. We find strong evidence that quality Tasmanian summer (DJF) streamflow reconstructions based on tree-rings are possible. Evidence also suggests that streamflow reconstructions for other seasons are also likely to be possible, especially as additional chronologies based on wood properties such as tracheid radial diameter, microfibril angle, density and cell wall thickness become available. Based on the relationships between streamflows and tree-ring chronologies, and between streamflows and major precipitation drivers across Australia, we conclude that Tasmanian tree-ring chronologies are likely to prove useful as predictors for seasonal streamflow reconstructions, particularly in eastern Australia. Successful streamflow reconstructions for a much broader portion of Australia than currently available will be invaluable for future water resource management and planning. (C) 2015 Elsevier Ltd. All rights reserved.
机译:澳大利亚干燥的大陆经常遭受毁灭性的​​区域干旱,这使得高质量的古水文重建对于水资源管理和规划至关重要。在世界的其他地方,年轮构成了这种重建的核心组成部分。然而,对于澳大利亚的大部分地区来说,每年都无法确定的由树木年轮构成的古水文重建。最南端的塔斯马尼亚岛州是一个重要的例外,有超过50种树木年轮可用。驱使整个澳大利亚大陆降水的海洋-大气耦合过程也影响塔斯马尼亚的降水。在这里,我们提供了有关塔斯马尼亚季节性流量的重要驱动因素与潜在的流量预测因素(如树木年轮年代学)之间的地理关系如何将塔斯马尼亚的树木年轮预测因素的空间适用性扩展到当地背景之外的基础分析。我们在塔斯马尼亚流中发现了明确的地理和季节定义的模式,这些模式反映在塔斯马尼亚树年轮个体年表及其与流之间的关系中。我们发现有力的证据表明,基于树轮的高质量塔斯马尼亚夏季(DJF)流量重建是可能的。证据还表明,其他季节的水流重建也是可能的,尤其是随着基于木材特性(如气管径向直径,微纤丝角,密度和细胞壁厚度)的其他年代出现时。基于流量与树木年轮年代之间的关系,以及整个澳大利亚的流量与主要降水驱动因素之间的关系,我们得出结论,塔斯马尼亚树木年轮的年代可能被证明是季节性流量重建的预测指标,特别是在澳大利亚东部。与目前可用的方法相比,在澳大利亚更广阔的地区成功进行河流改建对于未来的水资源管理和规划而言将是无价的。 (C)2015 Elsevier Ltd.保留所有权利。

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