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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Do atmospheric teleconnection patterns explain variations and trends in thermal growing season parameters in Finland?
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Do atmospheric teleconnection patterns explain variations and trends in thermal growing season parameters in Finland?

机译:大气遥相关模式是否解释了芬兰热生季参数的变化和趋势?

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摘要

Using daily mean temperature datasets applied at regular grid points (10 x 10 km(2)) throughout Finland for the period 1961-2011, interannual variations and trends in thermal growing season (GS) parameters, in terms of start (GSS), end (GSE) and length (GSL) and their relationships with various atmospheric teleconnection patterns (ATPs) were analysed. The GSL in Finland naturally increases from north to south, in association with earlier GSS and later GSE. However, the results showed that during the last 50 years, GSL on national scale in Finland significantly (p < 0.05) increased, at a rate of 0.30 +/- 0.18 days year(-1). This change was mainly attributable to earlier GSS (0.16 +/- 0.13 days year-1, p < 0.05). The East Atlantic/West Russia (EA/WR) pattern was the most significant ATP influencing variations in GSS (rho = 0.33), GSE (rho =-0.42) and GSL (rho =-0.33) on national scale in Finland. Statistically significant (p<0.05) trends in GSL were all positive (increasing) and mainly observed in the centre (Oulu), upper east (Kuopio) andwest (Jyvaskyla), north (Rovaniemi-Sodankyla) and south-west coastal areas (Helsinki-Turku-Vaasa) of Finland. Increasing GSL in central, upper eastern and western Finland was mainly associated with significantly earlier GSS; that in the north with significantly later GSE; and that in the most south-westerly areas with both earlier GSS and later GSE. These increases in GSL and corresponding shifts in GSS and/or GSE were significantly correlated with the East Atlantic (EA) pattern in northern and central Finland; with the EA/WR pattern in the south, south-east and south-west; and with the North Atlantic Oscillation (NAO) and the Arctic Oscillation (AO) in south-west coastal areas. The results provide a detailed national and spatial picture of changes in GS parameters in Finland during the last 50 years and reveal that the interannual variability in GS parameters in Finland is strongly linked with a number of ATPs, such as the EA, EA/WR, NAO and AO.
机译:使用1961-2011年期间在芬兰常规栅格点(10 x 10 km(2))上应用的每日平均温度数据集,以开始(GSS),结束时间为单位的热生长季节(GS)参数的年际变化和趋势(GSE)和长度(GSL)及其与各种大气遥相关模式(ATP)的关系进行了分析。芬兰的GSL与较早的GSS和较晚的GSE一起自然地从北向南增加。但是,结果显示,在过去的50年中,芬兰的国家级GSL显着增加(p <0.05),年增长率为0.30 +/- 0.18天(-1)。这种变化主要归因于较早的GSS(第1年0.16 +/- 0.13天,p <0.05)。在芬兰国家范围内,东大西洋/俄罗斯西部(EA / WR)模式是影响GSS(rho = 0.33),GSE(rho = -0.42)和GSL(rho = -0.33)的最重要的ATP变化。 GSL的统计上显着(p <0.05)趋势均为正(增加),并且主要观察到中部(奥卢),上东部(Kuopio)和西部(于韦斯屈莱),北部(罗瓦涅米-苏丹基拉)和西南沿海地区(赫尔辛基) -Turku-Vaasa)。芬兰中部,上东部和西部地区GSL的增加主要与GSS明显提前有关。北部的GSE明显晚一些;以及最西南的地区,同时拥有较早的GSS和较晚的GSE。 GSL的增加以及GSS和/或GSE的相应变化与芬兰北部和中部的东大西洋(EA)模式显着相关;在南部,东南部和西南部具有EA / WR模式;以及西南沿海地区的北大西洋涛动(NAO)和北极涛动(AO)。结果提供了过去50年来芬兰GS参数变化的详细的国家和空间图片,并揭示了芬兰GS参数的年际变化与许多ATP(例如EA,EA / WR, NAO和AO。

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