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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Developing large-scale forcing data for single-column and cloud-resolving models from the Mixed-Phase Arctic Cloud Experiment
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Developing large-scale forcing data for single-column and cloud-resolving models from the Mixed-Phase Arctic Cloud Experiment

机译:通过混合相北极云实验为单柱和云解析模型开发大规模强迫数据

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摘要

This study represents an effort to develop Single-Column Model (SCM) and Cloud-Resolving Model large-scale forcing data from a sounding array in the high latitudes. An objective variational analysis approach is used to process data collected from the Atmospheric Radiation Measurement Program (ARM) Mixed-Phase Arctic Cloud Experiment (M-PACE), which was conducted over the North Slope of Alaska in October 2004. In this method the observed surface and top of atmosphere measurements are used as constraints to adjust the sounding data from M-PACE in order to conserve column-integrated mass, heat, moisture, and momentum. Several important technical and scientific issues related to the data analysis are discussed. It is shown that the analyzed data reasonably describe the dynamic and thermodynamic features of the Arctic cloud systems observed during M-PACE. Uncertainties in the analyzed forcing fields are roughly estimated by examining the sensitivity of those fields to uncertainties in the upper-air data and surface constraints that are used in the analysis. Impacts of the uncertainties in the analyzed forcing data on SCM simulations are discussed. Results from the SCM tests indicate that the bulk features of the observed Arctic cloud systems can be captured qualitatively well using the forcing data derived in this study, and major model errors can be detected despite the uncertainties that exist in the forcing data as illustrated by the sensitivity tests. Finally, the possibility of using the European Center for Medium-Range Weather Forecasts analysis data to derive the large-scale forcing over the Arctic region is explored.
机译:这项研究代表着从高纬度测深阵列开发单列模型(SCM)和云解析模型大规模强迫数据的努力。客观变分分析方法用于处理2004年10月在阿拉斯加北坡进行的大气辐射测量程序(ARM)混合相北极云实验(M-PACE)收集的数据。大气表面和顶部的测量值用作约束条件,以调整M-PACE的测深数据,以节省色谱柱的质量,热量,湿度和动量。讨论了与数据分析有关的几个重要的技术和科学问题。结果表明,所分析的数据合理地描述了在M-PACE期间观测到的北极云系统的动力学和热力学特征。通过检查这些场对高空数据不确定性和分析中使用的地面约束的敏感性,可以粗略地估算出所分析的强迫场中的不确定性。讨论了所分析的强迫数据中的不确定性对单片机仿真的影响。 SCM测试的结果表明,使用本研究得出的强迫数据可以很好地定性捕获观测到的北极云系统的大部分特征,尽管强迫数据中存在不确定性,但仍可以检测到主要的模型误差,如下图所示。敏感性测试。最后,探讨了使用欧洲中距离天气预报中心分析数据得出北极地区大规模强迫的可能性。

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