首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Interannual variability of European extreme winter rainfall and links with mean large-scale circulation
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Interannual variability of European extreme winter rainfall and links with mean large-scale circulation

机译:欧洲极端冬季降水的年际变化及其与平均大尺度环流的联系

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摘要

December-February (DJF) extreme rainfall was analysed at 347 European stations for the period 1958-2000. Two indices of extreme rainfall were examined: the maximum number of consecutive dry days (CDD); and the number of days above the 1961-90 90th percentile of wet-day amounts (R90N). A principal component analysis of CDD found six components that accounted for 52.4% of the total variance. Six components of DJF R90N were also retained that accounted for 39.1% of the total variance. The second component of R90N has a very significant trend and the factor loadings closely resemble the observed linear trend in this index, suggesting that the analysis has isolated the mode of variability causing the trend as a separate component. The principal components of the indices were correlated with surface and upper-air observations over the North Atlantic. The best correlations were generally found to be with sea-level pressure (SLP) observations. A separate canonical correlation analysis of each of the two indices with SLP revealed several coupled modes of variability. The North Atlantic oscillation (NAO) was isolated as the first canonical pattern for R90N. For CDD the first two canonical coefficients of CDD were significantly correlated with the NAO index. Generally, the canonical coefficients with the highest correlations with the NAO had the most significant trends, suggesting that the observed trend in the NAO has strongly contributed to the observed trends in the indices. Two other important canonical patterns were isolated: a pattern of anomalous mean SLP (MSLP) centred over the North Sea, which seems to be related to local sea-surface temperature over this region; and a dipole-like pattern of MSLP with poles over the eastern Mediterranean and the central North Atlantic. Repeating the canonical correlation analysis with two other indices of extreme rainfall, the 90th percentile of wet day amounts and the maximum 10 day rainfall total, gives very similar coupled patterns.
机译:在1958-2000年期间,对347个欧洲站点的12月至2月(DJF)极端降雨进行了分析。检查了两个极端降雨指数:最大连续干旱天数(CDD);以及高于1961-90年第90个百日位数的天数(R90N)。 CDD的主成分分析发现六个成分占总方差的52.4%。 DJF R90N的六个组件也被保留,占总差异的39.1%。 R90N的第二个成分具有非常显着的趋势,并且因子负荷与该指数中观察到的线性趋势非常相似,这表明该分析已将导致该趋势的变化模式分离为一个单独的成分。该指数的主要成分与北大西洋上空的地面和高空观测值相关。通常发现最佳相关性与海平面压力(SLP)观测值有关。使用SLP对两个指标中的每一个进行单独的规范相关分析,揭示了几种耦合的变异性模式。北大西洋振荡(NAO)被隔离为R90N的第一个典型模式。对于CDD,CDD的前两个规范系数与NAO指数显着相关。通常,与NAO相关性最高的规范系数具有最显着的趋势,这表明NAO的观测趋势对指数的观测趋势有很大贡献。隔离了另外两个重要的规范模式:一种以北海为中心的异常平均SLP(MSLP)模式,它似乎与该地区的局部海表温度有关; MSLP呈偶极子状,其极点位于地中海东部和北大西洋中部。用其他两个极端降雨指数重复进行规范的相关性分析,即湿日数量的第90个百分位数和最大10天的降雨总量,得出的耦合模式非常相似。

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