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Statistical emulation of streamflow projections from a distributed hydrological model: Application to CMIP3 and CMIP5 climate projections for British Columbia, Canada

机译:来自分布式水文模型的流流投影的统计仿真:在加拿大不列颠哥伦比亚省的CMIP3和CMIP5气候投影的应用

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摘要

A recent hydrological impacts study in British Columbia, Canada, used an ensemble of 23 climate change simulations to assess potential future changes in streamflow. These Coupled Model Intercomparison Project Phase 3 (CMIP3) simulations were statistically downscaled and used to drive the Variable Infiltration Capacity (VIC) hydrology model over several watersheds. Due to computational restrictions, the 23 member VIC ensemble is a subset of the full 136 member CMIP3 archive. Extending the VIC ensemble to cover the full range of uncertainty represented by CMIP3, and incorporating the latest generation CMIP5 ensembles, poses a considerable computing challenge. Thus, we extend the VIC ensemble using a computationally efficient statistical emulation model, which approximates the combined output of the two-step process of statistical downscaling and hydrologic modeling, trained with the 23 member VIC ensemble. Regularized multiple linear regression links projected changes in monthly temperature and precipitation with projected changes in monthly streamflow over the Fraser and Peace River watersheds. Following validation, the statistical emulator is forced with the full suite of CMIP3 and CMIP5 climate change projections. The 23 member VIC ensemble has a smaller spread than the full ensemble; however, both ensembles provide the same consensus estimate of monthly streamflow change. Qualitatively, CMIP5 shows a similar streamflow response as CMIP3 for snow-dominated hydrologic regimes. However, by end-century, the CMIP5 worst-case RCP8.5 has a larger impact than CMIP3 A2. This work also underscores the advantage of using emulation to rapidly identify those future extreme projections that may merit further study using more computationally demanding process-based methods.
机译:最近在不列颠哥伦比亚省的水文影响研究加拿大,使用了23个气候变化模拟的集合来评估流流的潜在未来变化。这些耦合型号互通项目第3阶段3(CMIP3)模拟在统计上缩小并用于驱动多个流域的可变渗透能力(VIC)水文模型。由于计算限制,23个成员VIC集合是完整的136成员CMIP3档案的子集。扩展VIC集合以涵盖CMIP3所代表的全部不确定性,并结合最新一代CMIP5集合,构成了相当大的计算挑战。因此,我们使用计算有效的统计仿真模型扩展VIC集合,其近似于统计缩小和水文建模的两步过程的组合输出,用23构件VIC集合训练。正常化的多个线性回归链接预计每月温度和降水的变化,并在弗雷泽和和平河流域的每月流动流量的预计变化。在验证之后,统计模拟器用全套CMIP3和CMIP5气候变化预测强制。 23个成员VIC集合具有比整个集合更小的差价;但是,两个合奏都提供了每月流流程变化的相同共识估计。定性地,CMIP5显示了与CMIP3相似的流流响应,用于恐吓水文制度。然而,通过结束 - 世纪,CMIP5最坏情况RCP8.5的影响比CMIP3 A2更大。这项工作还强调了使用仿真以快速识别可能使用更多基于过程的基于过程的方法的进一步研究的未来极端预测的优点。

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  • 来源
    《Water resources research》 |2014年第11期|8907-8926|共20页
  • 作者单位

    Univ Victoria Pacific Climate Impacts Consortium Victoria BC Canada;

    Univ Victoria Pacific Climate Impacts Consortium Victoria BC Canada;

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  • 正文语种 eng
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