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HEAT WAVES IN THE ROMANIAN CARPATHIANS DURING THE COLD SEASON

机译:寒冷季节罗马尼亚喀尔巴阡山脉的热浪

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摘要

Heat waves are a representative index frequently used to analyse the incidence of extreme temperature in a given area. A study was undertaken on the frequency and duration of such phenomena in the Romanian Carpathians during the cold season (September 30-May 31). The STARDEX heat wave definition used reads that: there should be at least five consecutive days with daily maximum temperature deviations higher than 5°C from the multiannual average of the day taken into consideration. Investigations had in view the mountain weather stations located >1,000 m above sea level (27 locations) over the 1961-2007 period. Regional patterns of heat waves were expressed by comparing their severity in terms of persistence for the weather stations located both in the alpine, sub-alpine and forest vegetation belts. The results indicated significant increasing frequency trends of heat wave duration associated to the high temperature anomalies recorded during the cold season, especially in the last quarter of the 20th century and after 2000. Low altitude mountain sites are generally most affected by heat wave occurrence.
机译:热波是一个代表性指标,经常用于分析给定区域中极端温度的发生率。在寒冷季节(9月30日至5月31日),对罗马尼亚喀尔巴阡山脉中此类现象的发生频率和持续时间进行了研究。使用的STARDEX热波定义为:至少应该连续五天,每天的最大温度偏差要比所考虑的一天的多年平均值高出5°C以上。调查表明,1961-2007年期间,山地气象站位于海拔> 1,000 m处(27个位置)。通过比较它们在高山,亚高山和森林植被带上气象站的持久性的严重程度来表示热浪的区域模式。结果表明,与寒冷季节记录的高温异常相关的热波持续时间的频率趋势显着增加,尤其是在20世纪最后四分之一和2000年之后。低海拔山区通常受热波影响最大。

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