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Improvements of numerical weather predictions using a new AVHRR green vegetation fraction dataset

机译:使用新的AVHRR绿色植被分数数据集的数值天气预报的改进

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This study aims to analyze impacts of the NESDIS new product of green vegetation fraction (GVF) data on simulated surface air temperature and surface fluxes over the continental United States (CONUS) using the Nonhydrostatic Mesoscale Model (NMM) core of the Weather Research and Forecasting (WRF) system, i.e. WRF-NMM, coupled with the Noah land surface model (LSM). The new global 0.144 by 0.144 degree GVF dataset is an AVHHR-based, near realtime weekly dataset starting from 1982. It has better quality and a higher temporal resolution than the old monthly GVF dataset that is currently used in the NOAA operational numerical weather prediction models. The new weekly climatology GVF data shows a higher percentage of greenness fraction over most US areas than the old dataset, with the largest differences by 20-40% over the southeast U.S., the northern Middle West, and the west coast of California in summer. We have performed some case studies over CONUS during July 2006. In general, using the new GVF data cools predicted surface temperature over most regions compared to the old data, with the largest cooling over regions with the largest GVF increase. The latent heat increases significantly over most areas while the sensible heat decreases slightly. These results are physically consistent as more of the net radiation is dissipated in form of latent heat via enhanced evapotranspiration in response to increasing vegetation cover. Compared with observations, the new GVF application reduces the WRF-NMM 2-m surface air temperature warm biases, 2-m relative humidity negative biases, and their RMSEs.
机译:本研究旨在利用天气研究和预测的非水疗法Mesoscale模型(NMM)核心,分析绿色植被分数(GVF)数据对大陆美国(康明斯)的模拟表面空气温度和表面磁通量的影响(WRF)系统,即WRF-NMM,与诺亚陆地表面模型(LSM)相结合。新的全球0.144乘0.144度GVF数据集是一个基于AVHR的RealTime每周数据集,从1982年开始。它具有比NOAA操作数值天气预报模型目前使用的旧月GVF数据集更好的质量和更高的时间分辨率。新的每周气候学GVF数据都显示出比旧数据集的大多数地区的绿色级数更高,差异最大,在夏季加州的东南部,北中西部和西海岸的差异最大20-40%。我们在2006年7月进行了一定的案例研究。一般来说,与旧数据相比,使用新的GVF数据在大多数地区预测地面温度降低了表面温度,在最大的GVF地区的区域上最大的冷却。在大多数区域上,潜热显着增加,而显着的热量略有下降。这些结果在物理上是一致的,随着更多的净辐射通过增强的蒸发而通过增强的蒸散散,响应于增加的植被覆盖而散发。与观察结果相比,新的GVF应用降低了WRF-NMM 2-M表面空气温度温暖偏差,2-M相对湿度负偏差,以及其RMS。

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