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Framework for exploration of climatic and landscape controls on catchment water balance, with emphasis on inter-annual variability

机译:探索关于流域水平衡的气候和景观控制的框架,重点是年际变化

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This paper presents a systematic examination of the process controls on inter-annual variability of annual water balance. A simple, linear rainfall-runoff model is used for this purpose, in combination with idealised patterns of within-year variability of rainfall. The effects of these intra-annual patterns of variability of climate (e.g., storminess, seasonality) on annual water balance are examined through the simulation of annual runoff in three semi-arid catchments located in Queensland, South Australia and Western Australia, and one temperate catchment in New Zealand. A simple lumped model, that includes saturation excess overland flow and subsurface stormflow, is used, via sensitivity analyses with respect to different aspects of the infra-annual variability (i.e., seasonality and storminess). In the Queensland catchment storminess is found to be the dominant factor, whereas in Western Australia and South Australia seasonality is found to be the dominant climate control. In wetter catchments (e.g., New Zealand), the water balance is relatively insensitive to soil properties, whereas in dry places (e.g., Western Australia and South Australia) the water balance is highly sensitive to soil properties, such as the soil depth, confirming the results of previous modelling studies. The insights gained from this study can assist in the deciphering of the vast complexity of observed inter-annual variability of catchment responses in terms of their underlying process controls, which can be valuable towards the development of parsimonious water balance models.
机译:本文对年度水平衡的年际变化过程控制进行了系统的研究。为此,使用了一个简单的线性降雨-径流模型,并结合了年内降雨变化的理想模式。通过模拟位于昆士兰州,南澳大利亚州和西澳大利亚州的三个半干旱集水区和一个温带地区的年径流量,研究了这些年际气候变化(例如,暴风雨,季节性)年度变化模式对年度水平衡的影响。新西兰的集水区。通过对年际变化的不同方面(即季节性和暴风雨)进行敏感性分析,使用了一个简单的集总模型,该模型包括饱和过量的陆上流量和地下风暴流量。在昆士兰流域,暴风雨是主要的控制因素,而在西澳大利亚和南澳大利亚,季节性是主要的气候控制因素。在潮湿的流域(例如新西兰),水平衡对土壤特性相对不敏感,而在干燥的地方(例如西澳大利亚州和南澳大利亚),水平衡对土壤特性(例如土壤深度)高度敏感,这证明了先前建模研究的结果。从这项研究中获得的见识可以帮助根据其潜在的过程控制来解释所观察到的流域响应的年际变化的巨大复杂性,这对于开发简约的水平衡模型可能是有价值的。

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