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Tests of precipitation parameterizations available in latest version of NCAR regional climate model (RegCM) over continental United States

机译:美国大陆上最新版本的NCAR区域气候模型(RegCM)中提供的降水参数化测试

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This paper presents a series of tests of resolvable scale precipitation and cumulus convection schemes available in the latest version of the NCAR regional climate model (RegCM). For resolvable scale precipitation we use a new simplified explicit moisture (SIMEX) scheme, while for cumulus convection, we test the mass-flux scheme of Grell [1993], the Kuo-type scheme of Anthes [1977], and the newly implemented scheme of Zhang and McFarlane [1995]. The period of simulation is 3 years long, from March 1993 to February 1996, and the domain covers the continental United States at 60 km resolution. When using the SIMEX and Grell schemes, the model shows the best performance, with generally good simulation of precipitation, surface air temperature, and large-scale circulations throughout the United States. Both averages and anomalies associated with individual seasons are well reproduced at the regional scale. Main model deficiences are an underestimate of cold season precipitation over the eastern United States and a displacement of the summer precipitation maximum over the central plains. The Kuo scheme has a performance more similar to that of the Grell scheme than that of the Zhang and McFarlane (ZMF) scheme. Use of the ZMF scheme yields a reasonably good simulation of regionally averaged precipitation, but deteriorates some aspect of the simulation such as the intensity of the summer low-level jet over the central plains. We also present sensitivity tests to various parameters in the schemes which can be of guidance to the model user for optimizing the model performance over different regions.
机译:本文介绍了最新版本的NCAR区域气候模型(RegCM)中可用的可分辨尺度降水和积云对流方案的一系列测试。对于可解决的规模降水,我们使用新的简化显式湿度(SIMEX)方案,对于积云对流,我们测试Grell [1993]的质量通量方案,Anthes [1977]的Kuo型方案以及新实施的方案Zhang and McFarlane [1995]。从1993年3月到1996年2月,模拟期为3年,该域以60 km的分辨率覆盖美国大陆。当使用SIMEX和Grell方案时,该模型表现出最佳性能,并且在整个美国范围内对降水,地表空气温度和大规模环流进行了总体良好的模拟。与单个季节相关的平均值和异常值在区域范围内均得到很好的再现。主要的模型缺陷是低估了美国东部的寒冷季节降水量以及中部平原上夏季降水最大值的位移。与Zhang和McFarlane(ZMF)方案相比,Kuo方案的性能与Grell方案更相似。使用ZMF方案可以对区域平均降水进行合理的模拟,但会破坏模拟的某些方面,例如中部平原上夏季低空急流的强度。我们还提出了对方案中各种参数的敏感性测试,可以为模型用户在不同区域优化模型性能提供指导。

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