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Regional analysis of extreme temperature and precipitation indices for the Carpathian Basin from 1946 to 2001

机译:1946年至2001年喀尔巴阡盆地极端温度和降水指数的区域分析

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Since human and natural systems may be especially affected by changes of extreme climate events, the main objective of our research is to detect the possible changes of intensity and frequency of these extreme events. Several climate extreme indices are analyzed and compared for Central/Eastern Europe (focusing on Hungary) for the 20th century based on the guidelines suggested by the joint WMO-CCl/CLIVAR Working Group on climate change detection. These climate extreme indices include the numbers of severe cold days, winter days, frost days, cold days, warm days, summer days, hot days, extremely hot days, cold nights, warm nights, hot nights, the intra-annual extreme temperature range, the heat wave duration, the number of wet days (using several threshold values defining extremes, i.e., 10 mm and 20 mm), the maximum number of consecutive dry days, the highest 1-day precipitation amount, the greatest 5-day rainfall total, the simple daily precipitation intensity, the numbers of moderate wet days and very wet days, the annual fraction due to extreme precipitation events, etc. Therefore, daily maximum, minimum and mean temperature observations (from 13 stations) and daily precipitation amounts (from 31 stations) are used in the present statistical analysis. Our results suggest that similarly to the global and continental trends, regional temperature of Central/Eastern Europe has become warmer during the second half of the 20th century. Specifically, the strongest increasing tendency is detected in case of the annual numbers of hot days, summer days, warm days, warm nights, and the heat wave duration index. Before this warming period in the last quarter of the 20th century, most of the indices exhibit a cooling period until the middle of the 1970's. Furthermore, regional intensity and frequency of extreme precipitation has increased (as shown by the annual fraction due to extreme precipitation events, and the numbers of moderate wet days, very wet days, and very heavy precipitation days) between 1976 and 2001, while the total precipitation has decreased (as shown by numbers of precipitation days exceeding 0.1 mm, 1 mm, and 5 mm) in the region.
机译:由于人类和自然系统可能特别受到极端气候事件变化的影响,因此我们研究的主要目的是检测这些极端事件强度和频率的可能变化。根据WMO-CCl / CLIVAR联合气候变化工作组建议的指南,分析并比较了20世纪中欧(东欧)(匈牙利)的几个极端气候指数。这些气候极端指数包括严寒天,冬季天,霜冻天,寒冷天,温暖天,夏季天,炎热天,极热天,寒冷的夜晚,温暖的夜晚,炎热的夜晚,年内极端温度范围的数量,热浪持续时间,潮湿天数(使用定义极限值的几个阈值,即10 mm和20 mm),最大连续干燥天数,最高1天降水量,最大5天降水量总的来说,简单的日降水强度,中湿天和极湿天的数量,由于极端降水事件引起的年分数等。因此,每天的最高,最低和平均温度观测值(来自13个站点)和每日降水量(来自31个台站的数据)用于本次统计分析。我们的结果表明,与全球和大陆趋势类似,中欧/东欧的区域温度在20世纪下半叶变得更暖。具体而言,在每年的炎热天,夏季天,温暖的日子,温暖的夜晚和热浪持续时间指数的情况下,检测到最强的增长趋势。在20世纪最后四分之一的变暖时期之前,大多数指数都处于冷却期,直到1970年代中期。此外,1976年至2001年之间,极端降水的区域强度和频率增加了(如极端降水事件引起的年分数以及中度湿日,极湿日和极重日的数量),而该地区的降水减少了(如降水天数超过0.1毫米,1毫米和5毫米)。

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