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The northern hemisphere circumglobal teleconnection in a seasonal forecast model and its relationship to European summer forecast skill

机译:北半球环绕全球遥相关的季节预报模型及其与欧洲夏季预报技能的关系

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Forecasting seasonal variations in European summer weather represents a considerable challenge. Here, we assess the performance of a seasonal forecasting model at representing a major mode of northern hemisphere summer climate variability, the circumglobal teleconnection (CGT), and the implications of errors in its representation on seasonal forecasts for the European summer (June, July, August). Using seasonal hindcasts initialised at the start of May, we find that the model skill for forecasting the interannual variability of 500 hPa geopotential height is poor, particularly over Europe and several other centres of action of the CGT. The model also has a weaker CGT pattern than is observed, particularly in August, when the observed CGT wavetrain is strongest. We investigate several potential causes of this poor skill. First, model variance in geopotential height in west-central Asia (an important region for the maintenance of the CGT) is lower than observed in July and August, associated with a poor representation of the link between this region and Indian monsoon precipitation. Second, analysis of the Rossby wave source shows that the source associated with monsoon heating is both too strong and displaced to the northeast in the model. This is related to errors in monsoon precipitation over the Bay of Bengal and Arabian Sea, where the model has more precipitation than is observed. Third, the model jet is systematically shifted northwards by several degrees latitude over large parts of the northern hemisphere, which may affect the propagation characteristics of Rossby waves in the model.
机译:预测欧洲夏季天气的季节性变化是一个巨大的挑战。在这里,我们评估了代表北半球夏季气候变异的主要模式,环球全球遥相关(CGT)的季节预报模型的性能,以及在欧洲夏季(6月,7月,八月)。使用5月初初始化的季节性后兆,我们发现预测500 hPa地势高度年际变化的模型技能很差,尤其是在欧洲和CGT的其他几个行动中心。该模型的CGT模式也比所观察到的要弱,尤其是在8月,此时所观察到的CGT波列最强。我们调查了这种技能低下的几种潜在原因。首先,中西部亚洲(CGT维持的重要区域)的地势高度模型差异低于7月和8月的观测值,这与该地区与印度季风降水之间联系的代表性较差有关。其次,对Rossby波源的分析表明,与季风加热有关的源太强,并且在模型中向东北移动。这与孟加拉湾和阿拉伯海上的季风降水误差有关,那里的降水比实际观测到的要多。第三,模型射流在北半球的大部分区域系统地向北移动了数个纬度,这可能会影响模型中Rossby波的传播特性。

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