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Spatial and temporal variability of extreme precipitation in poland in the period 1951-2006

机译:1951-2006年波兰极端降水的时空变化

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摘要

The study investigated spatial and temporal variability of extreme precipitation trend magnitudes and their directions. Daily precipitation from 48 synoptic stations in Poland for the period 1951-2006 were used. Five indices of precipitation extremes were chosen: the highest 5-day precipitation total, precipitation total from events ≥90th and 95th percentiles as well as number of days with precipitation ≥90th and 95th percentiles of daily precipitation amount. Trends in extreme precipitation indicators were analysed over semi-annual periods as well as over the standard climatological seasons. Trends were calculated for each of the 30-year moving periods within 1951-2006 using a simple linear regression method. Their significance was tested with the Mann-Kendall method. Decreasing trends in extreme precipitation indices dominated in both the warm and cool halves of the year and in the seasons. The greatest change was recorded in the least extreme precipitation indices. Summer was the season with the greatest number of statistically significant trends, mostly decreasing ones. Upward trends, having the greatest spatial extend in autumn, dominated the initial 30-year periods of the study period whereas the decreasing trends were common in the 30-years from 1956. In summer and winter, decreasing trends reached the greatest degrees of stability in southern Poland. In spring and autumn, a stable fall of extreme precipitation indices was mainly recorded in the south-western part of the country. Stable increasing trends were recorded sporadically. However, in spring trends towards an increase were more frequent than in other seasons. The strongest decreasing trends were observed in summer and winter, mainly in the south, while in autumn they also occurred in the west.
机译:该研究调查了极端降水趋势幅度及其方向的时空变化。使用了1951-2006年间波兰48个天气站的日降水量。选择了五个极端降水指数:最高的5天降水总量,≥90和95%百分数的事件的降水总量以及降水量≥日降水量的90%和95%的日数。在半年期和标准气候季节内分析了极端降水指标的趋势。使用简单的线性回归方法计算了1951年至2006年这30年的每个移动周期的趋势。他们的意义用曼恩-肯德尔方法进行了检验。极端降水指数的下降趋势在一年中的两个季节和季节的两个季节均占主导地位。最大的变化记录在最小极端降水指数中。夏季是统计上具有显着趋势的数量最多的季节,大部分呈下降趋势。上升趋势在秋天具有最大的空间扩展,主导了研究期的最初30年,而下降趋势在1956年以来的30年中很常见。在夏季和冬季,下降趋势达到了最大的稳定性。波兰南部。在春季和秋季,极端降水指数的稳定下降主要记录在该国西南部。零星记录稳定的增长趋势。但是,春季的增长趋势比其他季节更为频繁。夏季和冬季下降趋势最明显,主要发生在南部,而秋季则出现在西部。

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