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Sensitivity studies of high-resolution RegCM3 simulations of precipitation over the European Alps: the effect of lateral boundary conditions and domain size

机译:高分辨率RegCM3模拟对欧洲阿尔卑斯山降水的敏感性研究:横向边界条件和区域尺寸的影响

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摘要

A suite of high-resolution (10 km) simulations were performed with the International Centre for Theoretical Physics (ICTP) Regional Climate Model (RegCM3) to study the effect of various lateral boundary conditions (LBCs), domain size, and intermediate domains on simulated precipitation over the Great Alpine Region. The boundary conditions used were ECMWF ERA-Interim Reanalysis with grid spacing 0.75(ay), the ECMWF ERA-40 Reanalysis with grid spacing 1.125 and 2.5(ay), and finally the 2.5(ay) NCEP/DOE AMIP-II Reanalysis. The model was run in one-way nesting mode with direct nesting of the high-resolution RCM (horizontal grid spacing Delta x = 10 km) with driving reanalysis, with one intermediate resolution nest (Delta x = 30 km) between high-resolution RCM and reanalysis forcings, and also with two intermediate resolution nests (Delta x = 90 km and Delta x = 30 km) for simulations forced with LBC of resolution 2.5(ay). Additionally, the impact of domain size was investigated. The results of multiple simulations were evaluated using different analysis techniques, e.g., Taylor diagram and a newly defined useful statistical parameter, called Skill-Score, for evaluation of daily precipitation simulated by the model. It has been found that domain size has the major impact on the results, while different resolution and versions of LBCs, e.g., 1.125(ay) ERA40 and 0.7(ay) ERA-Interim, do not produce significantly different results. It is also noticed that direct nesting with reasonable domain size, seems to be the most adequate method for reproducing precipitation over complex terrain, while introducing intermediate resolution nests seems to deteriorate the results.
机译:与国际理论物理中心(ICTP)区域气候模型(RegCM3)一起进行了一组高分辨率(10 km)模拟,以研究各种侧向边界条件(LBC),区域大小和中间区域对模拟的影响大高山地区的降水。使用的边界条件是网格间距为0.75(ay)的ECMWF ERA-临时再分析,网格间距为1.125和2.5(ay)的ECMWF ERA-40再分析,最后是2.5(ay)NCEP / DOE AMIP-II再分析。该模型在单向嵌套模式下运行,其中直接嵌套高分辨率RCM(水平网格间距Delta x = 10 km),并进行驱动重新分析,在高分辨率RCM之间有一个中等分辨率嵌套(Delta x = 30 km)以及重新分析的强制,以及两个中间分辨率嵌套(Delta x = 90 km和Delta x = 30 km),用于使用分辨率为2.5(ay)的LBC强制进行的模拟。此外,研究了域大小的影响。使用不同的分析技术(例如泰勒图)和新定义的有用统计参数(称为Skill-Score)对多次模拟的结果进行评估,以评估模型模拟的每日降水量。已经发现,域大小对结果有主要影响,而不同分辨率和不同版本的LBC,例如1.125(ay)ERA40和0.7(ay)ERA-Interim,不会产生明显不同的结果。还应注意的是,以合理的域大小进行直接嵌套似乎是在复杂地形上再现降水的最合适方法,而引入中分辨率嵌套似乎会使结果恶化。

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  • 来源
    《Theoretical and applied climatology》 |2016年第4期|617-630|共14页
  • 作者

    Nadeem Imran; Formayer Herbert;

  • 作者单位

    Univ Nat Resources & Life Sci Vienna BOKU, Inst Meteorol, Vienna, Austria;

    Univ Nat Resources & Life Sci Vienna BOKU, Inst Meteorol, Vienna, Austria;

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  • 正文语种 eng
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