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首页> 外文期刊>Geophysical Research Letters >Climatological validation of stratospheric temperatures in ECMWF operational analyses with CHAMP radio occultation data - art. no. L12806
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Climatological validation of stratospheric temperatures in ECMWF operational analyses with CHAMP radio occultation data - art. no. L12806

机译:利用CHAMP无线电掩星数据在ECMWF运行分析中对平流层温度进行气候学验证-艺术。没有。 L12806

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摘要

A climatological validation of the thermal structure of European Centre for Medium-Range Weather Forecasts (ECMWF) operational analyses with a new 2.5-year dataset derived from the CHAllenging Minisatellite Payload (CHAMP) radio occultation (RO) satellite mission was performed. Close overall agreement was found in the 10 30 km altitude region, with seasonal zonal mean temperature biases generally smaller than 0.5 K. Apart from that, discrepancies in the Austral polar vortex region ( cold biases up to - 2.5 K, warm biases up to + 3.5 K) and a cold bias of the analysis at the low-latitude tropopause ( up to - 2 K) were revealed. The polar vortex bias can be clearly attributed to the ECMWF analysis and data assimilation system and the tropopause bias is strongly indicated to be related to the smaller tropopause variability and the lower vertical resolution in the analysis. The study underlines the utility of RO data as global long-term climate reference datasets.
机译:对欧洲中型天气预报中心(ECMWF)运行分析的热结构进行了气候学验证,并使用了一个新的2.5年数据集,该数据集来自挑战微型卫星有效载荷(CHAMP)无线电掩星(RO)卫星任务。在海拔10 30 km的区域发现总体上接近一致,季节性纬向平均温度偏差通常小于0.5K。此外,南极涡旋区的差异(冷偏差高达-2.5 K,暖偏差高达+揭示了在低纬度对流层顶(高达-2 K)时分析的冷偏差(3.5 K)。极地涡旋偏差可以清楚地归因于ECMWF分析和数据同化系统,强烈指出对流层顶偏斜与较小的对流层顶变异性和较低的垂直分辨率有关。这项研究强调了反渗透数据作为全球长期气候参考数据集的实用性。

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