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Rapid Retrieval and Assimilation of Ground Based GPS Precipitable Water Observations at the NOAA Forecast Systems Laboratory: Impact on Weather Forecasts

机译:在NOAA预报系统实验室中对地面GPS可沉淀水的观测值进行快速检索和同化:对天气预报的影响

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Since 1994, the NOAA Research-Forecast Systems Laboratory (NOAA/FSL) has been evaluating the utility of ground-based Global Positioning System (GPS) remote sensing techniques for operational weather forecasting, climate monitoring, atmospheric research, and other applications such as satellite calibration and validation. Techniques have been developed to acquire, process, distribute GPS integrated precipitable water vapor (IPW) retrievals and ancillary surface meteorological observations every 30-minutes with less than 15 minute latency. Techniques to assimilate these observations into the research version of the Rapid Update Cycle (RUC) numerical weather prediction assimilation/model system running hourly at NOAA/FSL have been developed, and the impacts of these observations on shortrange weather forecast accuracy have been evaluated since 1998 using a 60-km version of the system. These assessments consist of data denial experiments (parallel runs with and without GPS water vapor observations) to determine the impact that GPS-derived integrated (or total column) precipitable water vapor (IPW) retrievals have on short-range moisture and precipitation forecasts. The experiments have been conducted over a portion of the central United States that, from a meteorological perspective, is one of the best-observed areas on Earth. While this greatly facilitates the impact assessments, it also presents a special challenge to a new observing system under evaluation, such as GPS-Met, since relatively few measurements have to “compete” with an enormous number of other (conventional and nonconventional) observations of similar and related parameters. Despite this, five years of experiments in- dicate more or less continuous improvements in 3-hour relative humidity forecasts at pressure levels below 500 hPa. The greatest skill is seen during the cold season when moisture changes are dominated by synoptic-scale weather systems. Perhaps the most significant result is that the impact in improved forecast skill from assimilation of GPS-IPW data has increased each year as the number of stations has increased, suggesting that further increases in the network density over the United States will result in further forecast improvement.
机译:自1994年以来,NOAA研究预报系统实验室(NOAA / FSL)一直在评估地面全球定位系统(GPS)遥感技术在运营天气预报,气候监测,大气研究以及卫星等其他应用中的实用性校准和验证。已经开发出了每30分钟获取,处理,分配GPS集成的可沉淀水蒸气(IPW)检索和辅助地面气象观测的技术,且延迟少于15分钟。已开发出将这些观测值同化为每小时在NOAA / FSL运行的快速更新周期(RUC)数值天气预报同化/模型系统的研究版本的技术,并且自1998年以来已评估了这些观测值对短时天气预报准确性的影响使用60公里版本的系统。这些评估包括数据拒绝实验(有无GPS水蒸气观测的平行运行),以确定GPS衍生的集成(或总柱)可沉淀水蒸气(IPW)取回对短期水分和降水预报的影响。实验已在美国中部部分地区进行,从气象学角度来看,该地区是地球上观察得最好的地区之一。尽管这极大地促进了影响评估,但它也给正在评估的新观测系统(例如GPS-Met)带来了特殊挑战,因为相对较少的测量就必须与大量其他(常规和非常规)观测“竞争”相似和相关的参数。尽管如此,五年的实验表明,在低于500 hPa的压力下,3小时相对湿度的预报或多或少地得到了持续改善。在寒冷季节,天气变化最主要的是湿度,而天气变化是天气系统的主导。也许最重要的结果是,随着台站数量的增加,GPS-IPW数据的同化对提高预报技能的影响每年都在增加,这表明美国网络密度的进一步提高将导致进一步的预报改进。

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