Accounting for precipitation asymmetry in a multiplicative random cascade disaggregation model

IF 5.7 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Hydrology and Earth System Sciences Pub Date : 2023-10-18 DOI:10.5194/hess-27-3643-2023
Kaltrina Maloku, Benoit Hingray, Guillaume Evin
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引用次数: 1

Abstract

Abstract. Analytical multiplicative random cascades (MRCs) are widely used for the temporal disaggregation of coarse-resolution precipitation time series. This class of models applies scaling models to represent the dependence of the cascade generator on the temporal scale and the precipitation intensity. Although determinant, the dependence on the external precipitation pattern is usually disregarded in the analytical scaling models. Our work presents a unified MRC modelling framework that allows the cascade generator to depend in a continuous way on the temporal scale, precipitation intensity and a so-called precipitation asymmetry index. Different MRC configurations are compared for 81 locations in Switzerland with contrasted climates. The added value of the dependence of the MRC on the temporal scale appears to be unclear, unlike what was suggested in previous works. Introducing the precipitation asymmetry dependence into the model leads to a drastic improvement in model performance for all statistics related to precipitation temporal persistence (wet–dry transition probabilities, lag-n autocorrelation coefficients, lengths of dry–wet spells). Accounting for precipitation asymmetry seems to solve this important limitation of previous MRCs. The model configuration that only accounts for the dependence on precipitation intensity and asymmetry is highly parsimonious, with only five parameters, and provides adequate performances for all locations, seasons and temporal resolutions. The spatial coherency of the parameter estimates indicates a real potential for regionalisation and for further application to any location in Switzerland.
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在乘法随机级联分解模型中考虑降水不对称性
摘要解析乘法随机级联(MRCs)被广泛用于粗分辨率降水时间序列的时间分解。这类模型采用尺度模型来表示梯级发生器对时间尺度和降水强度的依赖关系。虽然是决定性的,但在解析标度模型中通常忽略了对外部降水模式的依赖。我们的工作提出了一个统一的MRC建模框架,该框架允许级联发生器以连续的方式依赖于时间尺度、降水强度和所谓的降水不对称指数。不同的MRC配置比较了81个地点在瑞士的对比气候。与之前的研究不同,MRC在时间尺度上的依赖性的附加价值似乎不清楚。在模型中引入降水不对称依赖会导致与降水时间持久性相关的所有统计数据(干湿转换概率、滞后自相关系数、干湿期长度)的模型性能的急剧改善。考虑降水不对称似乎解决了以前MRCs的这一重要限制。仅考虑降水强度和不对称性依赖的模式配置非常简洁,只有5个参数,并提供了所有地点、季节和时间分辨率的足够性能。参数估计的空间一致性表明了区域化和进一步应用于瑞士任何地点的真正潜力。
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来源期刊
Hydrology and Earth System Sciences
Hydrology and Earth System Sciences 地学-地球科学综合
CiteScore
10.10
自引率
7.90%
发文量
273
审稿时长
15 months
期刊介绍: Hydrology and Earth System Sciences (HESS) is a not-for-profit international two-stage open-access journal for the publication of original research in hydrology. HESS encourages and supports fundamental and applied research that advances the understanding of hydrological systems, their role in providing water for ecosystems and society, and the role of the water cycle in the functioning of the Earth system. A multi-disciplinary approach is encouraged that broadens the hydrological perspective and the advancement of hydrological science through integration with other cognate sciences and cross-fertilization across disciplinary boundaries.
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