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The accuracy of stratospheric analyses in the northern hemisphere inferred from long-duration balloon flights

机译:从长期气球飞行推断北半球平流层分析的准确性

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In January and February 2002, six superprcssure balloons (SPBs) were launched from Kiruna, Sweden (69°N, 21°E). The balloons drifted in the polar lower stratosphere for up to 45 days. Temperature, wind and altitude observations wore collected every15 minutes during the Mights. This dataset scries as a reference to assess the accuracy of the European Centre for Medium-Range Weather Forecasts (ECMWF) analyses and the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalyzes in the lower stratosphere during the 2002 winter. In particular, it is found that both models succeeded in simulatinsi the large temperature fluctuations observed during the SPB flights, which were induced by a ideographical shift between the stratospheric vortex and the low temperature area. Furthermore, the model biases are found to be small for all variables (temperature, wind, height). Nevertheless, it is found that NCEP/NCAR reanalvses tend to be slightly wanner (0.8 K) than the observations, while the converse is true for ECMWF analyses (--0.3 K). The observations also exhibit small-scale fluctuations that are presumably produced by (inertia-) gravity waves and which induce some scatter in the analysis/observation comparisons. Finally, trajectory comparisons are performed. It is found that trajectories built with ECMWF vv inds are more accurate than those built with NCEP/NCAR winds. With both models, the trajectory errors increase with lime upto about 15 days and thentend to fluctuate. Typical errors after 15 days are 1000 ± l200 km for F.CMWF and 2300 ± 1300 km for NCHP trajectories.
机译:2002年1月和2002年2月,从瑞典基律纳(北纬69°,东经21°)发射了六个超高压气球(SPB)。气球在极地平流层下层漂浮了长达45天。战斗期间每15分钟收集一次温度,风向和高度的观测值。该数据集旨在评估2002年欧洲中距离天气预报中心(ECMWF)分析和国家环境预测中心/国家大气研究中心(NCEP / NCAR)在平流层下层进行的重新分析的准确性。冬季。特别是,发现两个模型都成功地模拟了SPB飞行期间观察到的大的温度波动,这是由平流层涡旋和低温区域之间的表意变化引起的。此外,发现所有变量(温度,风,高度)的模型偏差都较小。但是,发现NCEP / NCAR重新分析往往比观测值略微偏弱(0.8 K),而ECMWF分析(--0.3 K)则相反。观测结果还显示出可能由(惯性)重力波产生的小规模波动,并且在分析/观测比较中引起了一些分散。最后,进行轨迹比较。发现使用ECMWF vv inds构建的轨迹比使用NCEP / NCAR风构建的轨迹更准确。在这两个模型中,轨迹误差都会随着石灰的增加而增加,最长持续约15天,并且波动的趋势也很大。 15天后的典型误差对于F.CMWF为1000±l200 km,对于NCHP轨迹为2300±1300 km。

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