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首页> 外文期刊>Tellus, Series A. Dynamic meteorology & oceanography >Temperature and precipitation during winter in Ny?lesund, Svalbard and possible tropical linkages
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Temperature and precipitation during winter in Ny?lesund, Svalbard and possible tropical linkages

机译:纽约冬季温度和降水?Lesund,Svalbard和可能的热带联系

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Winter (DJF) temperature and precipitation variability in an Arctic Archipelago, Svalbard is investigated for an extreme event during December 2015 as well as on interannual time scales. During December 2015–16, a strong high pressure anomaly over northern Europe channelised warm and moist air into Ny ?lesund (~79°N and ~11°E) resulting in extreme temperature and precipitation. This high pressure anomaly was a result of wave trains associated with the Madden Julian Oscillation (MJO). On interannual time scales, the observation site, Ny ?lesund was characterised by an increasing trend in precipitation and temperature. A composite of SLP anomalies associated with the temperature and precipitation anomalies was characterised by a high pressure anomaly over northern Europe. The second mode in the EOF of SLP anomalies during winter (DJF) also indicated the presence of a high pressure anomaly over northern Europe, extending into the Pacific. The mode was correlated significantly with the ENSO. During the study period, more than 50% of the ENSO events influenced temperature and precipitation in Ny Alesund. In the present study, the EOF-2 temporal pattern correlated strongly with La Nina in the Pacific, suggesting the generation of a high/low pressure anomaly during negative/positive ENSO phases. On interannual timescales, extremes were conspicuous, particularly when La Nina coincided with active MJO. This may be due to the fact that both processes generate similar pressure anomalies in northern Europe and reinforce each other. This study also suggests that the influence of El Nino is weaker than La Nina. It is also noted that decadal oscillations in the Pacific, particularly the Interdecadal Pacific Oscillation (IPO) also enhance the high-pressure anomalies over northern Europe. Thus, the temperature and precipitation in a high Arctic location, Ny ?lesund is interconnected, at least hemispherically and is defined by processes of different time scales.
机译:冬季(DJF)在北极群岛的温度和降水变异,斯瓦尔巴德于2015年12月和持续时间尺度调查了极端事件。在2015 - 15年12月期间,北欧的强大高压异常将温暖和潮湿的空气传播到NY?Lesund(〜79°N和〜11°E),导致极端的温度和沉淀。这种高压异常是与Madden Julian振荡(MJO)相关的波动列车的结果。在持续时间尺度,观察部位,NY?Lesund的特点是降水和温度的趋势。与温度和沉淀异常相关的SLP异常的复合物,其特征在于北欧高压异常。在冬季(DJF)期间SLP异常EOF中的第二种模式也表明存在于北欧的高压异常,延伸到太平洋。该模式与ENSO显着相关。在研究期间,超过50%的ENSO事件影响了NY Alesund的温度和降水。在本研究中,EOF-2时间模式与太平洋的LA NINA强烈相关,表明在负/阳性enso阶段期间产生高/低压异常。在际时间尺度上,极端是显眼的,特别是当La Nina恰逢活跃的MJO时。这可能是由于两种过程都在北欧产生了类似的压力异常,并互相加强。本研究还表明El Nino的影响比La Nina弱。还有人指出,太平洋地区的额外振荡,特别是跨跨越的太平洋振荡(IPO)还增强了北欧的高压异常。因此,在高北极位置NY中的温度和沉淀,纽约圈互连,至少半球形,并由不同时间尺度的过程定义。

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