...
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
【24h】

Evaluation of Polar WRF forecasts on the Arctic System Reanalysis domain: Surface and upper air analysis

机译:北极极地WRF评估预测系统再分析域:表面和高空分析

获取原文
获取原文并翻译 | 示例
           

摘要

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:3.1.1天气研究极地版本高分辨率和预测模型(WRF)区域范围内模型,用于模拟条件,2006年12月到11月2007. 近地表和对流层变量观测数据集。北极的系统再分析(ASR)与北极同化模型领域部分是由极地进行观察气象小组的伯德极地研究俄亥俄州立大学中心。在这个极WRF研究发展扩展的季节性海冰的进展反照率到整个北冰洋。最后条件规定NCEP全球网格分析存档(新兵)1°x 1°全球网格更新每6 h。模拟在48 h每日增量初始化执行0000 UTC,第一个24小时丢弃的模型向上的水文循环和边界层的过程。大气压力和位势高度显示良好的协议与观测。近地表气温的分布比较与ERA-Interim尽管很小负偏压在车站的分析。露点温度和风速显示小偏见,但模型技能是适度的近地表的风。然而,风速,同意与无线电探空仪观察。基准的改进模型指导极地WRF进一步发展ASR的主要模型。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号