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Diagnosis of the Source and Evolution of Medium-Range Forecast Errors for Extratropical Cyclone Joachim

机译:温带气旋约阿希姆中程预报误差的来源和演变诊断

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摘要

Medium-range forecasts for Cyclone Joachim, an extratropical cyclone that impacted western Europe on 16 December 2011, consistently predicted a high-impact intense cyclone; however, these forecasts failed to verify. The potential source and propagation of forecast errors for this case are diagnosed from the 51-member European Centre for Medium-Range Forecasts Ensemble Prediction System initialized 5 days prior to the cyclone's landfall. Ensemble members are subdivided into two groups: one that contained the eight members that had the most accurate forecast of Joachim and, the other, the eight members that predicted the most intense cyclone. Composite differences between these two subgroups indicate that the difference between these forecasts originate in tropopause-based subsynoptic waves along a deep trough in the eastern Pacific. These errors move eastward over a northern stream ridge centered on the west coast of North America and modulate the evolution of a trough that dives equatorward out of Canada and is associated with the development of Joachim. Forecast error calculations and relaxation experiments indicate that reducing forecast errors associated with these subsynoptic features leads to more accurate forecasts. These results present further evidence that subsynoptic errors, especially those originating in the warm sector of a cyclone, can be a significant source of downstream forecast errors.
机译:对2011年12月16日影响西欧的温带气旋Joachim旋风的中期预测始终预测到有强烈影响的强旋风。但是,这些预测未能得到验证。该事件的潜在误差来源和预报误差的传播是通过由51名成员组成的欧洲中距离预报预报系统的中心诊断的,该系统在飓风登陆前5天初始化。合奏成员分为两组:一组包含对Joachim预测最准确的八个成员,另一组包含对旋风最强烈的预测的八个成员。这两个亚组之间的综合差异表明,这些预测之间的差异源自东太平洋沿深槽的基于对流层顶的亚天气波。这些误差向北移动到以北美西海岸为中心的北部溪流山脊上,并调节了一条从赤道向加拿大外扩散并与约阿希姆的发展有关的海槽的演变。预报误差的计算和松弛实验表明,减少与这些亚天气特征有关的预报误差可导致更准确的预报。这些结果提供了进一步的证据,表明天气异常,特别是起源于气旋温暖带的天气异常,可能是下游预报误差的重要来源。

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