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Corrigendum to “Spatio‐temporal Variability and Trends in Extreme Temperature Events in Finland over the Recent Decades: Influence of Northern Hemisphere Teleconnection Patterns”

机译:近几十年来“芬兰极端温度事件的时空变异性和趋势的勘犯:北半球电信连接模式的影响”

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Fifteen temperature indices recommended by the ETCCDI (Expert Team on Climate Change Detection and Indices) were applied to evaluate spatiotemporal variability and trends in annual intensity, frequency, and duration of extreme temperature statistics in Finland during 1961–2011. Statistically significant relationships between these high-resolution (10?km) temperature indices and seven influential Northern Hemisphere teleconnection patterns (NHTPs) for the interannual climate variability were also identified. During the study period (1961–2011), warming trends in extreme temperatures were generally manifested by statistically significant increases in cold temperature extremes rather than in the warm temperature extremes. As expected, warm days and nights became more frequent, while fewer cold days and nights occurred. The frequency of frost and icing days also decreased. Finland experienced more (less) frequent warm (cold) temperature extremes over the past few decades. Significant lengthening in warm spells was observed in Finland during 1961–2011, while no clear changes are found in cold spells. Interannual variations in the temperature indices were significantly associated with a number of NHTPs. In general, warm temperature extremes show significant correlations with the East Atlantic and the Scandinavia patterns and cold temperature extremes with the Arctic Oscillation and the North Atlantic Oscillation patterns.
机译:ETCCDI(气候变化检测和指数专家团队推荐的十五个温度指数用于评估芬兰极端温度统计的年度强度,频率和持续时间的时空变异性和趋势。还识别出这些高分辨率(10 km)温度指数与七个有影响力的北半球联系模式(NHTPS)之间的统计学性质的统计学界也被识别出用于际气候变异性的七个影响。在研究期间(1961-2011)期间,极端温度的变暖趋势一般在静息极值的统计学上显着增加而不是在温热的温度极值中。正如预期的那样,温暖的日子和夜晚变得更加频繁,而发生了较少的寒冷日夜。霜冻和结冰日的频率也降低了。芬兰在过去几十年中经历了更多(较少)频繁的温暖(冷)温度极低。在1961 - 2011年,在芬兰观察到在芬兰观察到温暖法术的显着延长,而在寒冷的法术中没有发现明确的变化。温度指数的续际变化与许多NHTP有显着相关。一般来说,温暖的极端与东部大西洋和斯堪的纳维亚模式和寒冷的温度极值与北极振荡和北大西洋振荡模式的寒冷温度极为极值表现出显着的相关性。

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