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首页> 外文期刊>Quarterly Journal of the Royal Meteorological Society >Impact of model upgrades on diabatic processes in extratropical cyclones and downstream forecast evolution
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Impact of model upgrades on diabatic processes in extratropical cyclones and downstream forecast evolution

机译:模型升级对尿酸旋风区蛋白过程和下游预测演化的影响

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摘要

Models are continuously developed at numerical weather prediction (NWP) centres to improve forecast skill, with new operational model configurations adopted every few years. The parametrizations of diabatic processes are probably the most frequently updated part of NWP models as they are crucial for accurate weather predictions and contain uncertainties in their formulation. The impact of model developments is assessed here in forecasts from the Met Office's weather forecast model initialised throughout the North Atlantic Waveguide and Downstream Impact Experiment field campaign period in autumn 2016. Planned model parametrization developments are considered, together with an 'inexpensive coupled' forecast with daily updating of the sea surface temperature and sea-ice fraction. Forecasts produced from the coupled system have, on average, indistinguishable skill from the control forecasts, suggesting the benefits of coupled atmosphere-ocean NWP systems can be small. In contrast, a reduction in forecast error (similar to 4%) is identified in forecasts produced using an upgraded convection scheme. Periods of low forecast skill during the study period are shown to be associated with the onset and decay of blocking events and increased diabatic heating of air masses reaching the upper troposphere. In forecasts of a specific block development case that was not accurately predicted in any of the experiments or in the operational ensemble forecast from the Met Office, the representation of diabatic heating in the warm conveyor belt of an upstream cyclone is shown to moderate the subsequent block development; forecasts in which the heating is stronger generally have a more-amplified blocking ridge and amplified heating contributions from all parametrizations as diagnosed using diabatic tracers. Hence, we demonstrate that plausible changes to the representation of several different diabatic processes in models can impact forecast block development via changes within upstream cyclones.
机译:模型在数值天气预报(NWP)中心不断开发,以改善预测技能,每隔几年采用新的运营模型配置。糖尿病过程的参数化可能是NWP模型的最常见的部分,因为它们对于精确的天气预报至关重要,并且在其制定中包含不确定性。在2016年秋季的北大西洋波导和下游影响实验场竞选期内,梅特办公室天气预报模型的预测评估了模型发展的影响。计划模型参数化发展,与“廉价的耦合”预测一起考虑日常更新海面温度和海冰分数。从耦合系统产生的预测平均不可区分从对照预测中无法区分,表明耦合大气的益处 - 海洋NWP系统可以很小。相比之下,在使用升级的对流方案产生的预测中识别出预测误差(类似于4%)的减少。研究期间的低预测技能的时期显示出与阻塞事件的发作和衰减相关,并增加了到达上层对流层的空气肿块的延展热量。在预测到任何实验中未准确预测的特定块开发案例或从MOT办公室的操作集合预测中,显示在上游旋风器的温暖传送带中的糖尿病加热的表示中度适度发展;预测,加热更强通常具有更放大的阻塞脊和来自所有参数化的加热贡献,如使用糖尿病示踪剂所诊断的。因此,我们证明了模型中几种不同糖尿病过程的代表的合理变化可以通过上游旋风内的变化影响预测块开发。

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