...
首页> 外文期刊>Weather and forecasting >Evaluation of WRF Model Output for Severe Weather Forecasting from the 2008 NOAA Hazardous Weather Testbed Spring Experiment
【24h】

Evaluation of WRF Model Output for Severe Weather Forecasting from the 2008 NOAA Hazardous Weather Testbed Spring Experiment

机译:从2008年NOAA危险天气试验台春季试验评估严重天气预报的WRF模型输出。

获取原文
获取原文并翻译 | 示例
           

摘要

This study assesses forecasts of the preconvective and near-storm environments from the convectionallowing models run for the 2008 National Oceanic and Atmospheric Administration (NOAA) Hazardous Weather Testbed (HWT) spring experiment. Evaluating the performance of convection-allowing models (CAMs) is important for encouraging their appropriate use and development for both research and operations. Systematic errors in theCAMforecasts included a cold bias in mean 2-m and 850-hPa temperatures over most of the United States and smaller than observed vertical wind shear and 850-hPa moisture over the high plains. The placement of airmass boundaries was similar in forecasts from the CAMs and the operational North American Mesoscale (NAM) model that provided the initial and boundary conditions. This correspondence contributed to similar characteristics for spatial and temporalmean error patterns. However, substantial errors were found in the CAM forecasts away from airmass boundaries. The result is that the deterministic CAMs do not predict the environment as well as the NAM. It is suggested that parameterized processes used at convection-allowing grid lengths, particularly in the boundary layer, may be contributing to these errors. It is also shown that mean forecasts from an ensemble of CAMs were substantially more accurate than forecasts from deterministic CAMs. If the improvement seen in the CAM forecasts when going from a deterministic framework to an ensemble framework is comparable to improvements in mesoscale model forecasts when going from a deterministic to an ensemble framework, then an ensemble of mesoscale model forecasts could predict the environment even better than an ensemble of CAMs. Therefore, it is suggested that the combination of mesoscale (convection parameterizing) andCAMconfigurations is an appropriate avenue to explore for optimizing the use of limited computer resources for severe weather forecasting applications.
机译:这项研究通过为2008年美国国家海洋和大气管理局(NOAA)危险天气试验台(HWT)春季实验运行的对流允许模型评估了对流和近风暴环境的预测。评估对流允许模型(CAM)的性能对于鼓励其在研究和运营中的适当使用和开发非常重要。 CAM预报中的系统误差包括美国大部分地区平均2 m和850-hPa温度的冷偏差,小于观测到的垂直风切变和高平原上的850-hPa湿度。气层边界的位置在CAMs和提供初始条件和边界条件的北美中尺度运行(NAM)模型的预测中相似。这种对应关系为空间和时间平均误差模式提供了相似的特征。但是,在CAM预报中,在远离气团边界的地方发现了重大错误。结果是确定性CAM不能预测环境以及NAM。建议在对流允许网格长度(尤其是在边界层)中使用的参数化过程可能会导致这些误差。还显示,来自CAM集合的平均预测比确定性CAM的预测准确得多。如果从确定性框架转换为整体框架时CAM预测中看到的改进与从确定性框架转换为整体框架时中尺度模型预测的改进具有可比性,那么中尺度模型预测的整体预测环境可以比CAM的集合。因此,建议将中尺度(对流参数化)和CAM配置相结合是探索为严重天气预报应用优化有限计算机资源的使用的合适途径。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
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