利用气候遥相关随机生成东南澳大利亚似是而非的水文气候未来

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Journal of Hydrometeorology Pub Date : 2023-07-04 DOI:10.1175/jhm-d-22-0206.1
N. Potter, F. Chiew, D. Robertson
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引用次数: 0

摘要

生成可信的未来气候时间序列对于自下而上的气候影响建模以及水文应用的缩微气候模型输出都是必要的。基于气候遥相关时间序列(如IPO/SOI)与年降雨量之间的线性回归,基于亚年分解的碎片聚类方法,基于回归的日潜在蒸散(PET)水文建模方法,提出了一种生成多站点日随机气候序列的新方法。我们证明了偏差(即过采样)在多位点环境中与碎片分解的标准方法一起发生;并表明从聚类降雨量中选择一个模拟年比标准的片段方法具有更好的采样特性。利用澳大利亚东南部的水文数据,我们使用GR4J模型模拟观测和模拟降雨和PET的径流。新方法模拟的年和日降雨量和径流特征与现有方法相似,在湿-湿过渡概率和空间(站点间)相关性方面有所改进。
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Stochastic generation of plausible hydroclimate futures using climate teleconnections for South-Eastern Australia
Generating plausible future climate timeseries is needed for bottom-up climate impact modelling, as well as downscaling climate model output for hydrological applications. A novel method for generating multisite daily stochastic climate series is developed based on: 1) linear regression between climate teleconnection timeseries (e.g. IPO/SOI) and annual rainfall, 2) clustered method of fragments for subannual disaggregation, and 3) a regression-based approach to daily potential evapotranspiration (PET) for hydrological modelling. We demonstrate that bias (i.e. oversampling) occurs with the standard method of fragments disaggregation in the multisite context; and show that selection of an analogue year from clustered rainfall amounts provides better sampling properties than the standard method of fragments. Using hydrological data for south-eastern Australia, we model runoff from observed and simulated rainfall and PET using the GR4J model. Simulated annual and daily rainfall and runoff characteristics from the new method are similar to existing methods, with improvements demonstrated in wet-wet transition probabilities and spatial (between-site) correlations.
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来源期刊
Journal of Hydrometeorology
Journal of Hydrometeorology 地学-气象与大气科学
CiteScore
7.40
自引率
5.30%
发文量
116
审稿时长
4-8 weeks
期刊介绍: The Journal of Hydrometeorology (JHM) (ISSN: 1525-755X; eISSN: 1525-7541) publishes research on modeling, observing, and forecasting processes related to fluxes and storage of water and energy, including interactions with the boundary layer and lower atmosphere, and processes related to precipitation, radiation, and other meteorological inputs.
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