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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Dynamically and statistically downscaled seasonal temperature and precipitation hindcast ensembles for the southeastern USA
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Dynamically and statistically downscaled seasonal temperature and precipitation hindcast ensembles for the southeastern USA

机译:美国东南部的动态和统计缩减的季节性温度和降水后兆合奏

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摘要

We present results from a 15-year 10-member warm season (March-September) hindcast ensemble of maximum and minimum surface air temperatures and precipitation in southeast USA. The hindcasts are derived from the Florida State University/Center for Ocean-Atmospheric Prediction Studies Global Spectral Model (FSU/COAPS GSM) and downscaled using, both the FSU/COAPS Nested Regional Spectral Model (NRSM) and a statistical downscaling method based on stochastic weather generator techniques. We additionally consider statistical bias correction of the dynamical model output. Basic descriptive statistics indicate that the bias-corrected and statistically downscaled data reduce the FSU/COAPS GSM bias considerably in terms of basic climatology. Statistics describing the daily precipitation process are improved by both downscaling techniques relative to the bias-corrected GSM. Improvement in monthly and seasonal hindcasts relative to FSU/COAPS GSM is spatially and temporally varying. Precipitation hindcasts are generally less skillful than those for temperature, although useful precipitation predictability exists at many locations. Hindcast improvements due to downscaling are greatest over peninsular Florida. The smallest root mean square errors (RMSE) for temperature hindcasts are found in the southern part of the study region during the spring months of March, April and May (MAM) for maximum surface air temperature, and in the summer, June, July and August (JJA), for minimum Surface air temperature. Overall. there is no indication that either downscaling method has a direct advantage over the other. Copyright (c) 2008 Royal Meteorological Society
机译:我们介绍了美国东南部最大和最小地表气温和降水的15年10成员暖季(3月至9月)后播合奏的结果。后验数据来自佛罗里达州立大学/海洋大气预测研究中心全球光谱模型(FSU / COAPS GSM),并使用FSU / COAPS嵌套区域光谱模型(NRSM)和基于随机的统计缩减方法进行缩减天气生成器技术。我们还考虑了动力学模型输出的统计偏差校正。基本的描述性统计数据表明,就基本气候而言,经过偏差校正和统计缩减后的数据会大大降低FSU / COAPS GSM偏差。相对于经过偏差校正的GSM,两种降尺度技术均可改善描述每日降水过程的统计数据。与FSU / COAPS GSM相比,每月和季节性后播的改善在空间和时间上都在变化。尽管许多地方都存在有用的降水可预报性,但降水后预报通常不如温度预报好。由于规模缩小,Hindcast改进在佛罗里达州半岛上是最大的。在3月,4月和5月(MAM)的春季月份中,对于最高地面空气温度,以及在夏季,6月,7月和6月的春季,研究区域的南部发现了最低温度均方根误差(RMSE)。 8月(JJA),以确保最低地面空气温度。总体。没有迹象表明任何一种缩减方法都比另一种具有直接优势。版权所有(c)2008皇家气象学会

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