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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Evaluation of Polar WRF forecasts on the Arctic System Reanalysis domain: Surface and upper air analysis
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Evaluation of Polar WRF forecasts on the Arctic System Reanalysis domain: Surface and upper air analysis

机译:北极WRF预报在北极系统再分析领域的评估:地表和高空分析

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The Polar version 3.1.1 of the Weather Research and Forecasting model (WRF), a high-resolution regional scale model, is used to simulate conditions for the year December 2006 to November 2007. The goal is to compare model output of near-surface and tropospheric variables to observational data sets. The domain mirrors that of the Arctic System Reanalysis (ASR), an assimilation of model fields with Arctic observations being conducted partly by the Polar Meteorology Group of the Byrd Polar Research Center at Ohio State University. A key development in this Polar WRF study is the extension of the seasonal progression of sea ice albedo to the entire Arctic Ocean. The boundary conditions are specified by the NCEP Final global gridded analysis archive (FNL), a 1° x 1° global grid updated every 6 h. The simulations are performed in 48 h increments initialized daily at 0000 UTC, with the first 24 h discarded for model spin-up of the hydrologic cycle and boundary layer processes. Model large-scale variables of atmospheric pressure and geopotential height show good agreement with observations. Spatial distribution of near-surface air temperatures compares well with ERA-Interim despite a small negative bias in the station analysis. Surface dewpoint temperatures and wind speeds show small biases, but model skill is modest for near-surface winds. Tropospheric temperatures and wind speeds, however, agree well with radiosonde observations. This examination provides a benchmark from which to improve the model and guidance for further development of Polar WRF as ASR's primary model.
机译:天气研究和预报模型(WRF)的Polar版本3.1.1是高分辨率的区域尺度模型,用于模拟2006年12月至2007年11月的状况。目标是比较近地表的模型输出。和对流层变量到观测数据集。该域反映了北极系统再分析(ASR)的域,该模型域是通过俄亥俄州立大学伯德极地研究中心的极地气象学小组进行的,部分地与北极观测资料进行了同化。 Polar WRF研究的一项重要进展是将海冰反照率的季节性变化扩展到整个北冰洋。边界条件由NCEP最终全球网格分析存档(FNL)指定,每6小时更新1°x 1°的全局网格。以每天0000 UTC初始化的48 h增量执行模拟,丢弃前24 h以进行水文循环和边界层过程的模型旋转。大气压力和地势高度的大型模型变量与观测值显示出很好的一致性。尽管台站分析中的负偏差很小,但近地表空气温度的空间分布与ERA-Interim相当。地表露点温度和风速显示出较小的偏差,但模型技能对于近地表风是适度的。然而,对流层温度和风速与探空仪的观测结果非常吻合。这项检查提供了一个基准,可用来改进该模型,并为进一步开发Polar WRF作为ASR的主要模型提供指导。

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