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Study of the rain intensity in Athens and Thessaloniki, Greece

机译:关于雅典和希腊萨洛尼卡的降雨强度的研究

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In this study, the mean rain intensity (mm/h) in Athens and Thessaloniki,Greece, is examined during the period 1930–2007. The daily meteorologicaldata were acquired from the meteorological stations of the NationalObservatory of Athens (Thissio) and the University Campus of Thessaloniki.These stations have recorded the longest and reliable daily rain time seriesin Greece.The trends of the annual and seasonal mean, as well as the maximum rainintensity, are analyzed. On the one hand, all of the time series in Athenspresent higher figures of mean rain intensity during the period 1990–2007compared to the period 1930–1990. On the other hand, regarding the timeseries in Thessaloniki, the mean rain intensity remains in lower level thanthe respective one in Athens without significant trend at the ConfidenceLevel (CL) 95%. As far as the annual and seasonal maximum rainintensity is concerned, similar patterns appear. However, the summer maximumrain intensity in Thessaloniki remains at higher levels till 1970's. Theatmospheric circulation patterns for the extreme rain intensities showintense negative anomalies centred over Greece and positive anomalies to thenorth, with centre over Scandinavia.
机译:在这项研究中,考察了1930-2007年期间雅典和希腊塞萨洛尼基的平均降雨强度(mm / h)。每日气象数据是从雅典国家天文台(Thissio)和塞萨洛尼基大学校园的气象站获取的,这些站记录了希腊最长,最可靠的每日降雨时间序列。 每年和每年的趋势分析了季节性平均值以及最大降雨强度。一方面,与1930-1990年相比,雅典的所有时间序列在1990-2007年期间的平均降雨强度都较高。另一方面,关于塞萨洛尼基的时间序列,平均降雨强度保持在低于雅典相应水平的水平,而ConfidenceLevel(CL)95%时没有明显趋势。就年度和季节性最大降雨强度而言,出现了类似的模式。然而,塞萨洛尼基的夏季最大降雨强度一直保持较高水平,直到1970年代。极端降雨强度的大气环流模式显示,强烈的负异常集中在希腊上空,而正向异常集中在北侧,中心位于斯堪的纳维亚半岛。

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